Hemispherically symmetric strategies for stratospheric aerosol injection
<p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outc...
Ausführliche Beschreibung
Autor*in: |
Y. Zhang [verfasserIn] D. G. MacMartin [verfasserIn] D. Visioni [verfasserIn] E. M. Bednarz [verfasserIn] B. Kravitz [verfasserIn] |
---|
Format: |
E-Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2024 |
---|
Übergeordnetes Werk: |
In: Earth System Dynamics - Copernicus Publications, 2011, 15(2024), Seite 191-213 |
---|---|
Übergeordnetes Werk: |
volume:15 ; year:2024 ; pages:191-213 |
Links: |
Link aufrufen |
---|
DOI / URN: |
10.5194/esd-15-191-2024 |
---|
Katalog-ID: |
DOAJ098588117 |
---|
LEADER | 01000naa a22002652 4500 | ||
---|---|---|---|
001 | DOAJ098588117 | ||
003 | DE-627 | ||
005 | 20240413231859.0 | ||
007 | cr uuu---uuuuu | ||
008 | 240413s2024 xx |||||o 00| ||eng c | ||
024 | 7 | |a 10.5194/esd-15-191-2024 |2 doi | |
035 | |a (DE-627)DOAJ098588117 | ||
035 | |a (DE-599)DOAJc4aa7c056b2947bc948f28f71fa9c80a | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
050 | 0 | |a QE1-996.5 | |
050 | 0 | |a QE500-639.5 | |
100 | 0 | |a Y. Zhang |e verfasserin |4 aut | |
245 | 1 | 0 | |a Hemispherically symmetric strategies for stratospheric aerosol injection |
264 | 1 | |c 2024 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a Computermedien |b c |2 rdamedia | ||
338 | |a Online-Ressource |b cr |2 rdacarrier | ||
520 | |a <p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p< | ||
653 | 0 | |a Science | |
653 | 0 | |a Q | |
653 | 0 | |a Geology | |
653 | 0 | |a Dynamic and structural geology | |
700 | 0 | |a D. G. MacMartin |e verfasserin |4 aut | |
700 | 0 | |a D. Visioni |e verfasserin |4 aut | |
700 | 0 | |a E. M. Bednarz |e verfasserin |4 aut | |
700 | 0 | |a E. M. Bednarz |e verfasserin |4 aut | |
700 | 0 | |a E. M. Bednarz |e verfasserin |4 aut | |
700 | 0 | |a B. Kravitz |e verfasserin |4 aut | |
700 | 0 | |a B. Kravitz |e verfasserin |4 aut | |
773 | 0 | 8 | |i In |t Earth System Dynamics |d Copernicus Publications, 2011 |g 15(2024), Seite 191-213 |w (DE-627)638410703 |w (DE-600)2578793-7 |x 21904987 |7 nnns |
773 | 1 | 8 | |g volume:15 |g year:2024 |g pages:191-213 |
856 | 4 | 0 | |u https://doi.org/10.5194/esd-15-191-2024 |z kostenfrei |
856 | 4 | 0 | |u https://doaj.org/article/c4aa7c056b2947bc948f28f71fa9c80a |z kostenfrei |
856 | 4 | 0 | |u https://esd.copernicus.org/articles/15/191/2024/esd-15-191-2024.pdf |z kostenfrei |
856 | 4 | 2 | |u https://doaj.org/toc/2190-4979 |y Journal toc |z kostenfrei |
856 | 4 | 2 | |u https://doaj.org/toc/2190-4987 |y Journal toc |z kostenfrei |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_DOAJ | ||
912 | |a GBV_ILN_11 | ||
912 | |a GBV_ILN_20 | ||
912 | |a GBV_ILN_22 | ||
912 | |a GBV_ILN_23 | ||
912 | |a GBV_ILN_24 | ||
912 | |a GBV_ILN_31 | ||
912 | |a GBV_ILN_39 | ||
912 | |a GBV_ILN_40 | ||
912 | |a GBV_ILN_60 | ||
912 | |a GBV_ILN_62 | ||
912 | |a GBV_ILN_63 | ||
912 | |a GBV_ILN_65 | ||
912 | |a GBV_ILN_69 | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_73 | ||
912 | |a GBV_ILN_95 | ||
912 | |a GBV_ILN_105 | ||
912 | |a GBV_ILN_110 | ||
912 | |a GBV_ILN_151 | ||
912 | |a GBV_ILN_161 | ||
912 | |a GBV_ILN_170 | ||
912 | |a GBV_ILN_206 | ||
912 | |a GBV_ILN_213 | ||
912 | |a GBV_ILN_230 | ||
912 | |a GBV_ILN_267 | ||
912 | |a GBV_ILN_285 | ||
912 | |a GBV_ILN_293 | ||
912 | |a GBV_ILN_370 | ||
912 | |a GBV_ILN_602 | ||
912 | |a GBV_ILN_2003 | ||
912 | |a GBV_ILN_2005 | ||
912 | |a GBV_ILN_2009 | ||
912 | |a GBV_ILN_2011 | ||
912 | |a GBV_ILN_2014 | ||
912 | |a GBV_ILN_2055 | ||
912 | |a GBV_ILN_2108 | ||
912 | |a GBV_ILN_2111 | ||
912 | |a GBV_ILN_2119 | ||
912 | |a GBV_ILN_4012 | ||
912 | |a GBV_ILN_4037 | ||
912 | |a GBV_ILN_4112 | ||
912 | |a GBV_ILN_4125 | ||
912 | |a GBV_ILN_4126 | ||
912 | |a GBV_ILN_4249 | ||
912 | |a GBV_ILN_4305 | ||
912 | |a GBV_ILN_4306 | ||
912 | |a GBV_ILN_4307 | ||
912 | |a GBV_ILN_4313 | ||
912 | |a GBV_ILN_4322 | ||
912 | |a GBV_ILN_4323 | ||
912 | |a GBV_ILN_4324 | ||
912 | |a GBV_ILN_4325 | ||
912 | |a GBV_ILN_4338 | ||
912 | |a GBV_ILN_4367 | ||
912 | |a GBV_ILN_4700 | ||
951 | |a AR | ||
952 | |d 15 |j 2024 |h 191-213 |
author_variant |
y z yz d g m dgm d v dv e m b emb e m b emb e m b emb b k bk b k bk |
---|---|
matchkey_str |
article:21904987:2024----::eipeialsmerctaeisosrtshr |
hierarchy_sort_str |
2024 |
callnumber-subject-code |
QE |
publishDate |
2024 |
allfields |
10.5194/esd-15-191-2024 doi (DE-627)DOAJ098588117 (DE-599)DOAJc4aa7c056b2947bc948f28f71fa9c80a DE-627 ger DE-627 rakwb eng QE1-996.5 QE500-639.5 Y. Zhang verfasserin aut Hemispherically symmetric strategies for stratospheric aerosol injection 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p< Science Q Geology Dynamic and structural geology D. G. MacMartin verfasserin aut D. Visioni verfasserin aut E. M. Bednarz verfasserin aut E. M. Bednarz verfasserin aut E. M. Bednarz verfasserin aut B. Kravitz verfasserin aut B. Kravitz verfasserin aut In Earth System Dynamics Copernicus Publications, 2011 15(2024), Seite 191-213 (DE-627)638410703 (DE-600)2578793-7 21904987 nnns volume:15 year:2024 pages:191-213 https://doi.org/10.5194/esd-15-191-2024 kostenfrei https://doaj.org/article/c4aa7c056b2947bc948f28f71fa9c80a kostenfrei https://esd.copernicus.org/articles/15/191/2024/esd-15-191-2024.pdf kostenfrei https://doaj.org/toc/2190-4979 Journal toc kostenfrei https://doaj.org/toc/2190-4987 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 15 2024 191-213 |
spelling |
10.5194/esd-15-191-2024 doi (DE-627)DOAJ098588117 (DE-599)DOAJc4aa7c056b2947bc948f28f71fa9c80a DE-627 ger DE-627 rakwb eng QE1-996.5 QE500-639.5 Y. Zhang verfasserin aut Hemispherically symmetric strategies for stratospheric aerosol injection 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p< Science Q Geology Dynamic and structural geology D. G. MacMartin verfasserin aut D. Visioni verfasserin aut E. M. Bednarz verfasserin aut E. M. Bednarz verfasserin aut E. M. Bednarz verfasserin aut B. Kravitz verfasserin aut B. Kravitz verfasserin aut In Earth System Dynamics Copernicus Publications, 2011 15(2024), Seite 191-213 (DE-627)638410703 (DE-600)2578793-7 21904987 nnns volume:15 year:2024 pages:191-213 https://doi.org/10.5194/esd-15-191-2024 kostenfrei https://doaj.org/article/c4aa7c056b2947bc948f28f71fa9c80a kostenfrei https://esd.copernicus.org/articles/15/191/2024/esd-15-191-2024.pdf kostenfrei https://doaj.org/toc/2190-4979 Journal toc kostenfrei https://doaj.org/toc/2190-4987 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 15 2024 191-213 |
allfields_unstemmed |
10.5194/esd-15-191-2024 doi (DE-627)DOAJ098588117 (DE-599)DOAJc4aa7c056b2947bc948f28f71fa9c80a DE-627 ger DE-627 rakwb eng QE1-996.5 QE500-639.5 Y. Zhang verfasserin aut Hemispherically symmetric strategies for stratospheric aerosol injection 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p< Science Q Geology Dynamic and structural geology D. G. MacMartin verfasserin aut D. Visioni verfasserin aut E. M. Bednarz verfasserin aut E. M. Bednarz verfasserin aut E. M. Bednarz verfasserin aut B. Kravitz verfasserin aut B. Kravitz verfasserin aut In Earth System Dynamics Copernicus Publications, 2011 15(2024), Seite 191-213 (DE-627)638410703 (DE-600)2578793-7 21904987 nnns volume:15 year:2024 pages:191-213 https://doi.org/10.5194/esd-15-191-2024 kostenfrei https://doaj.org/article/c4aa7c056b2947bc948f28f71fa9c80a kostenfrei https://esd.copernicus.org/articles/15/191/2024/esd-15-191-2024.pdf kostenfrei https://doaj.org/toc/2190-4979 Journal toc kostenfrei https://doaj.org/toc/2190-4987 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 15 2024 191-213 |
allfieldsGer |
10.5194/esd-15-191-2024 doi (DE-627)DOAJ098588117 (DE-599)DOAJc4aa7c056b2947bc948f28f71fa9c80a DE-627 ger DE-627 rakwb eng QE1-996.5 QE500-639.5 Y. Zhang verfasserin aut Hemispherically symmetric strategies for stratospheric aerosol injection 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p< Science Q Geology Dynamic and structural geology D. G. MacMartin verfasserin aut D. Visioni verfasserin aut E. M. Bednarz verfasserin aut E. M. Bednarz verfasserin aut E. M. Bednarz verfasserin aut B. Kravitz verfasserin aut B. Kravitz verfasserin aut In Earth System Dynamics Copernicus Publications, 2011 15(2024), Seite 191-213 (DE-627)638410703 (DE-600)2578793-7 21904987 nnns volume:15 year:2024 pages:191-213 https://doi.org/10.5194/esd-15-191-2024 kostenfrei https://doaj.org/article/c4aa7c056b2947bc948f28f71fa9c80a kostenfrei https://esd.copernicus.org/articles/15/191/2024/esd-15-191-2024.pdf kostenfrei https://doaj.org/toc/2190-4979 Journal toc kostenfrei https://doaj.org/toc/2190-4987 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 15 2024 191-213 |
allfieldsSound |
10.5194/esd-15-191-2024 doi (DE-627)DOAJ098588117 (DE-599)DOAJc4aa7c056b2947bc948f28f71fa9c80a DE-627 ger DE-627 rakwb eng QE1-996.5 QE500-639.5 Y. Zhang verfasserin aut Hemispherically symmetric strategies for stratospheric aerosol injection 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p< Science Q Geology Dynamic and structural geology D. G. MacMartin verfasserin aut D. Visioni verfasserin aut E. M. Bednarz verfasserin aut E. M. Bednarz verfasserin aut E. M. Bednarz verfasserin aut B. Kravitz verfasserin aut B. Kravitz verfasserin aut In Earth System Dynamics Copernicus Publications, 2011 15(2024), Seite 191-213 (DE-627)638410703 (DE-600)2578793-7 21904987 nnns volume:15 year:2024 pages:191-213 https://doi.org/10.5194/esd-15-191-2024 kostenfrei https://doaj.org/article/c4aa7c056b2947bc948f28f71fa9c80a kostenfrei https://esd.copernicus.org/articles/15/191/2024/esd-15-191-2024.pdf kostenfrei https://doaj.org/toc/2190-4979 Journal toc kostenfrei https://doaj.org/toc/2190-4987 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 15 2024 191-213 |
language |
English |
source |
In Earth System Dynamics 15(2024), Seite 191-213 volume:15 year:2024 pages:191-213 |
sourceStr |
In Earth System Dynamics 15(2024), Seite 191-213 volume:15 year:2024 pages:191-213 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Science Q Geology Dynamic and structural geology |
isfreeaccess_bool |
true |
container_title |
Earth System Dynamics |
authorswithroles_txt_mv |
Y. Zhang @@aut@@ D. G. MacMartin @@aut@@ D. Visioni @@aut@@ E. M. Bednarz @@aut@@ B. Kravitz @@aut@@ |
publishDateDaySort_date |
2024-01-01T00:00:00Z |
hierarchy_top_id |
638410703 |
id |
DOAJ098588117 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">DOAJ098588117</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240413231859.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">240413s2024 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.5194/esd-15-191-2024</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ098588117</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJc4aa7c056b2947bc948f28f71fa9c80a</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QE1-996.5</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QE500-639.5</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Y. Zhang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Hemispherically symmetric strategies for stratospheric aerosol injection</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2024</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a"><p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p<</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Science</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Q</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Geology</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Dynamic and structural geology</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">D. G. MacMartin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">D. Visioni</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">E. M. Bednarz</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">E. M. Bednarz</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">E. M. Bednarz</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">B. Kravitz</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">B. Kravitz</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Earth System Dynamics</subfield><subfield code="d">Copernicus Publications, 2011</subfield><subfield code="g">15(2024), Seite 191-213</subfield><subfield code="w">(DE-627)638410703</subfield><subfield code="w">(DE-600)2578793-7</subfield><subfield code="x">21904987</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:15</subfield><subfield code="g">year:2024</subfield><subfield code="g">pages:191-213</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.5194/esd-15-191-2024</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/c4aa7c056b2947bc948f28f71fa9c80a</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://esd.copernicus.org/articles/15/191/2024/esd-15-191-2024.pdf</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2190-4979</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2190-4987</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_206</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2005</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2009</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2055</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2108</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2119</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4367</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">15</subfield><subfield code="j">2024</subfield><subfield code="h">191-213</subfield></datafield></record></collection>
|
callnumber-first |
Q - Science |
author |
Y. Zhang |
spellingShingle |
Y. Zhang misc QE1-996.5 misc QE500-639.5 misc Science misc Q misc Geology misc Dynamic and structural geology Hemispherically symmetric strategies for stratospheric aerosol injection |
authorStr |
Y. Zhang |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)638410703 |
format |
electronic Article |
delete_txt_mv |
keep |
author_role |
aut aut aut aut aut aut aut aut |
collection |
DOAJ |
remote_str |
true |
callnumber-label |
QE1-996 |
illustrated |
Not Illustrated |
issn |
21904987 |
topic_title |
QE1-996.5 QE500-639.5 Hemispherically symmetric strategies for stratospheric aerosol injection |
topic |
misc QE1-996.5 misc QE500-639.5 misc Science misc Q misc Geology misc Dynamic and structural geology |
topic_unstemmed |
misc QE1-996.5 misc QE500-639.5 misc Science misc Q misc Geology misc Dynamic and structural geology |
topic_browse |
misc QE1-996.5 misc QE500-639.5 misc Science misc Q misc Geology misc Dynamic and structural geology |
format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
cr |
hierarchy_parent_title |
Earth System Dynamics |
hierarchy_parent_id |
638410703 |
hierarchy_top_title |
Earth System Dynamics |
isfreeaccess_txt |
true |
familylinks_str_mv |
(DE-627)638410703 (DE-600)2578793-7 |
title |
Hemispherically symmetric strategies for stratospheric aerosol injection |
ctrlnum |
(DE-627)DOAJ098588117 (DE-599)DOAJc4aa7c056b2947bc948f28f71fa9c80a |
title_full |
Hemispherically symmetric strategies for stratospheric aerosol injection |
author_sort |
Y. Zhang |
journal |
Earth System Dynamics |
journalStr |
Earth System Dynamics |
callnumber-first-code |
Q |
lang_code |
eng |
isOA_bool |
true |
recordtype |
marc |
publishDateSort |
2024 |
contenttype_str_mv |
txt |
container_start_page |
191 |
author_browse |
Y. Zhang D. G. MacMartin D. Visioni E. M. Bednarz B. Kravitz |
container_volume |
15 |
class |
QE1-996.5 QE500-639.5 |
format_se |
Elektronische Aufsätze |
author-letter |
Y. Zhang |
doi_str_mv |
10.5194/esd-15-191-2024 |
author2-role |
verfasserin |
title_sort |
hemispherically symmetric strategies for stratospheric aerosol injection |
callnumber |
QE1-996.5 |
title_auth |
Hemispherically symmetric strategies for stratospheric aerosol injection |
abstract |
<p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p< |
abstractGer |
<p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p< |
abstract_unstemmed |
<p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p< |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 |
title_short |
Hemispherically symmetric strategies for stratospheric aerosol injection |
url |
https://doi.org/10.5194/esd-15-191-2024 https://doaj.org/article/c4aa7c056b2947bc948f28f71fa9c80a https://esd.copernicus.org/articles/15/191/2024/esd-15-191-2024.pdf https://doaj.org/toc/2190-4979 https://doaj.org/toc/2190-4987 |
remote_bool |
true |
author2 |
D. G. MacMartin D. Visioni E. M. Bednarz B. Kravitz |
author2Str |
D. G. MacMartin D. Visioni E. M. Bednarz B. Kravitz |
ppnlink |
638410703 |
callnumber-subject |
QE - Geology |
mediatype_str_mv |
c |
isOA_txt |
true |
hochschulschrift_bool |
false |
doi_str |
10.5194/esd-15-191-2024 |
callnumber-a |
QE1-996.5 |
up_date |
2024-07-03T18:07:57.432Z |
_version_ |
1803582258481725440 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">DOAJ098588117</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240413231859.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">240413s2024 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.5194/esd-15-191-2024</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ098588117</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJc4aa7c056b2947bc948f28f71fa9c80a</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QE1-996.5</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QE500-639.5</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Y. Zhang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Hemispherically symmetric strategies for stratospheric aerosol injection</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2024</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a"><p<Stratospheric aerosol injection (SAI) comes with a wide range of possible design choices, such as the location and timing of the injection. Different stratospheric aerosol injection strategies can yield different climate responses; therefore, understanding the range of possible climate outcomes is crucial to making informed future decisions on SAI, along with the consideration of other factors. Yet, to date, there has been no systematic exploration of a broad range of SAI strategies. This limits the ability to determine which effects are robust across different strategies and which depend on specific injection choices. This study systematically explores how the choice of SAI strategy affects climate responses in one climate model. Here, we introduce four hemispherically symmetric injection strategies, all of which are designed to maintain the same global mean surface temperature: an annual injection at the Equator (EQ), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 15° N and 15° S (15N<span class="inline-formula"<+</span<15S), an annual injection of equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N and 30° S (30N<span class="inline-formula"<+</span<30S), and a polar injection strategy that injects equal amounts of SO<span class="inline-formula"<<sub<2</sub<</span< at 60° N and 60° S only during spring in each hemisphere (60N<span class="inline-formula"<+</span<60S). We compare these four hemispherically symmetric SAI strategies with a more complex injection strategy that injects different quantities of SO<span class="inline-formula"<<sub<2</sub<</span< at 30° N, 15° N, 15° S, and 30° S in order to maintain not only the global mean surface temperature but also its large-scale horizontal gradients. All five strategies are simulated using version 2 of the Community Earth System Model with the middle atmosphere version of the Whole Atmosphere Community Climate model, version 6, as the atmospheric component, CESM2(WACCM6-MA), with the global warming scenario, Shared Socioeconomic Pathway (SSP)2-4.5. We find that the choice of SAI strategy affects the spatial distribution of aerosol optical depths, injection efficiency, and various surface climate responses. In addition, injecting in the subtropics produces more global cooling per unit injection, with the EQ and the 60N<span class="inline-formula"<+</span<60S cases requiring, respectively, 59 % and 50 % more injection than the 30N<span class="inline-formula"<+</span<30S case to meet the same global mean temperature target. Injecting at higher latitudes results in larger Equator-to-pole temperature gradients. While all five strategies restore Arctic September sea ice, the high-latitude injection strategy is more effective due to the SAI-induced cooling occurring preferentially at higher latitudes. These results suggest trade-offs wherein different strategies appear better or worse, depending on which metrics are deemed important.</p<</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Science</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Q</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Geology</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Dynamic and structural geology</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">D. G. MacMartin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">D. Visioni</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">E. M. Bednarz</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">E. M. Bednarz</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">E. M. Bednarz</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">B. Kravitz</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">B. Kravitz</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Earth System Dynamics</subfield><subfield code="d">Copernicus Publications, 2011</subfield><subfield code="g">15(2024), Seite 191-213</subfield><subfield code="w">(DE-627)638410703</subfield><subfield code="w">(DE-600)2578793-7</subfield><subfield code="x">21904987</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:15</subfield><subfield code="g">year:2024</subfield><subfield code="g">pages:191-213</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.5194/esd-15-191-2024</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/c4aa7c056b2947bc948f28f71fa9c80a</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://esd.copernicus.org/articles/15/191/2024/esd-15-191-2024.pdf</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2190-4979</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2190-4987</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_206</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2005</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2009</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2055</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2108</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2119</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4367</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">15</subfield><subfield code="j">2024</subfield><subfield code="h">191-213</subfield></datafield></record></collection>
|
score |
7.399686 |