Vegetation distribution on Tibetan Plateau under climate change scenario
Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In t...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhao, Dongsheng [verfasserIn] Wu, Shaohong [verfasserIn] Yin, Yunhe [verfasserIn] Yin, Zhi-Yong [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2011 |
|---|
| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: Regional Environmental Change - Springer-Verlag, 2001, 11(2011), 4 vom: 10. Mai, Seite 905-915 |
|---|---|
| Übergeordnetes Werk: |
volume:11 ; year:2011 ; number:4 ; day:10 ; month:05 ; pages:905-915 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10113-011-0228-7 |
|---|
| Katalog-ID: |
SPR008811172 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | SPR008811172 | ||
| 003 | DE-627 | ||
| 005 | 20201124052008.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 201005s2011 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.1007/s10113-011-0228-7 |2 doi | |
| 035 | |a (DE-627)SPR008811172 | ||
| 035 | |a (SPR)s10113-011-0228-7-e | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 100 | 1 | |a Zhao, Dongsheng |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Vegetation distribution on Tibetan Plateau under climate change scenario |
| 264 | 1 | |c 2011 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a Computermedien |b c |2 rdamedia | ||
| 338 | |a Online-Ressource |b cr |2 rdacarrier | ||
| 520 | |a Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau. | ||
| 650 | 4 | |a Vegetation distribution |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a BIOME4 model |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Tibetan Plateau |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Responses of vegetation to climate change |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Vegetation distribution |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Wu, Shaohong |e verfasserin |4 aut | |
| 700 | 1 | |a Yin, Yunhe |e verfasserin |4 aut | |
| 700 | 1 | |a Yin, Zhi-Yong |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Regional Environmental Change |d Springer-Verlag, 2001 |g 11(2011), 4 vom: 10. Mai, Seite 905-915 |w (DE-627)SPR008808457 |7 nnns |
| 773 | 1 | 8 | |g volume:11 |g year:2011 |g number:4 |g day:10 |g month:05 |g pages:905-915 |
| 856 | 4 | 0 | |u https://dx.doi.org/10.1007/s10113-011-0228-7 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_SPRINGER | ||
| 951 | |a AR | ||
| 952 | |d 11 |j 2011 |e 4 |b 10 |c 05 |h 905-915 | ||
| author_variant |
d z dz s w sw y y yy z y y zyy |
|---|---|
| matchkey_str |
zhaodongshengwushaohongyinyunheyinzhiyon:2011----:eeainitiuinnieapaeunecia |
| hierarchy_sort_str |
2011 |
| publishDate |
2011 |
| allfields |
10.1007/s10113-011-0228-7 doi (DE-627)SPR008811172 (SPR)s10113-011-0228-7-e DE-627 ger DE-627 rakwb eng Zhao, Dongsheng verfasserin aut Vegetation distribution on Tibetan Plateau under climate change scenario 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau. Vegetation distribution (dpeaa)DE-He213 BIOME4 model (dpeaa)DE-He213 Tibetan Plateau (dpeaa)DE-He213 Responses of vegetation to climate change (dpeaa)DE-He213 Vegetation distribution (dpeaa)DE-He213 Wu, Shaohong verfasserin aut Yin, Yunhe verfasserin aut Yin, Zhi-Yong verfasserin aut Enthalten in Regional Environmental Change Springer-Verlag, 2001 11(2011), 4 vom: 10. Mai, Seite 905-915 (DE-627)SPR008808457 nnns volume:11 year:2011 number:4 day:10 month:05 pages:905-915 https://dx.doi.org/10.1007/s10113-011-0228-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 11 2011 4 10 05 905-915 |
| spelling |
10.1007/s10113-011-0228-7 doi (DE-627)SPR008811172 (SPR)s10113-011-0228-7-e DE-627 ger DE-627 rakwb eng Zhao, Dongsheng verfasserin aut Vegetation distribution on Tibetan Plateau under climate change scenario 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau. Vegetation distribution (dpeaa)DE-He213 BIOME4 model (dpeaa)DE-He213 Tibetan Plateau (dpeaa)DE-He213 Responses of vegetation to climate change (dpeaa)DE-He213 Vegetation distribution (dpeaa)DE-He213 Wu, Shaohong verfasserin aut Yin, Yunhe verfasserin aut Yin, Zhi-Yong verfasserin aut Enthalten in Regional Environmental Change Springer-Verlag, 2001 11(2011), 4 vom: 10. Mai, Seite 905-915 (DE-627)SPR008808457 nnns volume:11 year:2011 number:4 day:10 month:05 pages:905-915 https://dx.doi.org/10.1007/s10113-011-0228-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 11 2011 4 10 05 905-915 |
| allfields_unstemmed |
10.1007/s10113-011-0228-7 doi (DE-627)SPR008811172 (SPR)s10113-011-0228-7-e DE-627 ger DE-627 rakwb eng Zhao, Dongsheng verfasserin aut Vegetation distribution on Tibetan Plateau under climate change scenario 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau. Vegetation distribution (dpeaa)DE-He213 BIOME4 model (dpeaa)DE-He213 Tibetan Plateau (dpeaa)DE-He213 Responses of vegetation to climate change (dpeaa)DE-He213 Vegetation distribution (dpeaa)DE-He213 Wu, Shaohong verfasserin aut Yin, Yunhe verfasserin aut Yin, Zhi-Yong verfasserin aut Enthalten in Regional Environmental Change Springer-Verlag, 2001 11(2011), 4 vom: 10. Mai, Seite 905-915 (DE-627)SPR008808457 nnns volume:11 year:2011 number:4 day:10 month:05 pages:905-915 https://dx.doi.org/10.1007/s10113-011-0228-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 11 2011 4 10 05 905-915 |
| allfieldsGer |
10.1007/s10113-011-0228-7 doi (DE-627)SPR008811172 (SPR)s10113-011-0228-7-e DE-627 ger DE-627 rakwb eng Zhao, Dongsheng verfasserin aut Vegetation distribution on Tibetan Plateau under climate change scenario 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau. Vegetation distribution (dpeaa)DE-He213 BIOME4 model (dpeaa)DE-He213 Tibetan Plateau (dpeaa)DE-He213 Responses of vegetation to climate change (dpeaa)DE-He213 Vegetation distribution (dpeaa)DE-He213 Wu, Shaohong verfasserin aut Yin, Yunhe verfasserin aut Yin, Zhi-Yong verfasserin aut Enthalten in Regional Environmental Change Springer-Verlag, 2001 11(2011), 4 vom: 10. Mai, Seite 905-915 (DE-627)SPR008808457 nnns volume:11 year:2011 number:4 day:10 month:05 pages:905-915 https://dx.doi.org/10.1007/s10113-011-0228-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 11 2011 4 10 05 905-915 |
| allfieldsSound |
10.1007/s10113-011-0228-7 doi (DE-627)SPR008811172 (SPR)s10113-011-0228-7-e DE-627 ger DE-627 rakwb eng Zhao, Dongsheng verfasserin aut Vegetation distribution on Tibetan Plateau under climate change scenario 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau. Vegetation distribution (dpeaa)DE-He213 BIOME4 model (dpeaa)DE-He213 Tibetan Plateau (dpeaa)DE-He213 Responses of vegetation to climate change (dpeaa)DE-He213 Vegetation distribution (dpeaa)DE-He213 Wu, Shaohong verfasserin aut Yin, Yunhe verfasserin aut Yin, Zhi-Yong verfasserin aut Enthalten in Regional Environmental Change Springer-Verlag, 2001 11(2011), 4 vom: 10. Mai, Seite 905-915 (DE-627)SPR008808457 nnns volume:11 year:2011 number:4 day:10 month:05 pages:905-915 https://dx.doi.org/10.1007/s10113-011-0228-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 11 2011 4 10 05 905-915 |
| language |
English |
| source |
Enthalten in Regional Environmental Change 11(2011), 4 vom: 10. Mai, Seite 905-915 volume:11 year:2011 number:4 day:10 month:05 pages:905-915 |
| sourceStr |
Enthalten in Regional Environmental Change 11(2011), 4 vom: 10. Mai, Seite 905-915 volume:11 year:2011 number:4 day:10 month:05 pages:905-915 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Vegetation distribution BIOME4 model Tibetan Plateau Responses of vegetation to climate change |
| isfreeaccess_bool |
false |
| container_title |
Regional Environmental Change |
| authorswithroles_txt_mv |
Zhao, Dongsheng @@aut@@ Wu, Shaohong @@aut@@ Yin, Yunhe @@aut@@ Yin, Zhi-Yong @@aut@@ |
| publishDateDaySort_date |
2011-05-10T00:00:00Z |
| hierarchy_top_id |
SPR008808457 |
| id |
SPR008811172 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR008811172</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20201124052008.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201005s2011 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10113-011-0228-7</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR008811172</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s10113-011-0228-7-e</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="100" ind1="1" ind2=" "><subfield code="a">Zhao, Dongsheng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Vegetation distribution on Tibetan Plateau under climate change scenario</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2011</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">Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vegetation distribution</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">BIOME4 model</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tibetan Plateau</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Responses of vegetation to climate change</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vegetation distribution</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wu, Shaohong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yin, Yunhe</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yin, Zhi-Yong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Regional Environmental Change</subfield><subfield code="d">Springer-Verlag, 2001</subfield><subfield code="g">11(2011), 4 vom: 10. Mai, Seite 905-915</subfield><subfield code="w">(DE-627)SPR008808457</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:11</subfield><subfield code="g">year:2011</subfield><subfield code="g">number:4</subfield><subfield code="g">day:10</subfield><subfield code="g">month:05</subfield><subfield code="g">pages:905-915</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s10113-011-0228-7</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</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_SPRINGER</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">11</subfield><subfield code="j">2011</subfield><subfield code="e">4</subfield><subfield code="b">10</subfield><subfield code="c">05</subfield><subfield code="h">905-915</subfield></datafield></record></collection>
|
| author |
Zhao, Dongsheng |
| spellingShingle |
Zhao, Dongsheng misc Vegetation distribution misc BIOME4 model misc Tibetan Plateau misc Responses of vegetation to climate change Vegetation distribution on Tibetan Plateau under climate change scenario |
| authorStr |
Zhao, Dongsheng |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)SPR008808457 |
| format |
electronic Article |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut |
| collection |
springer |
| remote_str |
true |
| illustrated |
Not Illustrated |
| topic_title |
Vegetation distribution on Tibetan Plateau under climate change scenario Vegetation distribution (dpeaa)DE-He213 BIOME4 model (dpeaa)DE-He213 Tibetan Plateau (dpeaa)DE-He213 Responses of vegetation to climate change (dpeaa)DE-He213 |
| topic |
misc Vegetation distribution misc BIOME4 model misc Tibetan Plateau misc Responses of vegetation to climate change |
| topic_unstemmed |
misc Vegetation distribution misc BIOME4 model misc Tibetan Plateau misc Responses of vegetation to climate change |
| topic_browse |
misc Vegetation distribution misc BIOME4 model misc Tibetan Plateau misc Responses of vegetation to climate change |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
cr |
| hierarchy_parent_title |
Regional Environmental Change |
| hierarchy_parent_id |
SPR008808457 |
| hierarchy_top_title |
Regional Environmental Change |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)SPR008808457 |
| title |
Vegetation distribution on Tibetan Plateau under climate change scenario |
| ctrlnum |
(DE-627)SPR008811172 (SPR)s10113-011-0228-7-e |
| title_full |
Vegetation distribution on Tibetan Plateau under climate change scenario |
| author_sort |
Zhao, Dongsheng |
| journal |
Regional Environmental Change |
| journalStr |
Regional Environmental Change |
| lang_code |
eng |
| isOA_bool |
false |
| recordtype |
marc |
| publishDateSort |
2011 |
| contenttype_str_mv |
txt |
| container_start_page |
905 |
| author_browse |
Zhao, Dongsheng Wu, Shaohong Yin, Yunhe Yin, Zhi-Yong |
| container_volume |
11 |
| format_se |
Elektronische Aufsätze |
| author-letter |
Zhao, Dongsheng |
| doi_str_mv |
10.1007/s10113-011-0228-7 |
| author2-role |
verfasserin |
| title_sort |
vegetation distribution on tibetan plateau under climate change scenario |
| title_auth |
Vegetation distribution on Tibetan Plateau under climate change scenario |
| abstract |
Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau. |
| abstractGer |
Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau. |
| abstract_unstemmed |
Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau. |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER |
| container_issue |
4 |
| title_short |
Vegetation distribution on Tibetan Plateau under climate change scenario |
| url |
https://dx.doi.org/10.1007/s10113-011-0228-7 |
| remote_bool |
true |
| author2 |
Wu, Shaohong Yin, Yunhe Yin, Zhi-Yong |
| author2Str |
Wu, Shaohong Yin, Yunhe Yin, Zhi-Yong |
| ppnlink |
SPR008808457 |
| mediatype_str_mv |
c |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/s10113-011-0228-7 |
| up_date |
2024-07-03T23:17:20.460Z |
| _version_ |
1803601723218984960 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR008811172</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20201124052008.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201005s2011 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10113-011-0228-7</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR008811172</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s10113-011-0228-7-e</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="100" ind1="1" ind2=" "><subfield code="a">Zhao, Dongsheng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Vegetation distribution on Tibetan Plateau under climate change scenario</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2011</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">Abstract The impact of climate change on distribution of vegetation is an important aspect in studies on the responses of ecosystems to the climate change. Particularly in the sensitive environments of the Tibetan Plateau, vegetation distribution may be significantly affected by climate change. In this research, the coupled biogeography and biogeochemistry model, BIOME4, was modified according to the features of vegetation distribution on the Plateau, and the Kappa statistic was used to evaluate the modeling results by comparing the simulated vegetation distribution with the existing 1:1,000,000 vegetation map of China. The comparison showed that modified model was appropriate for simulating the overall vegetation distribution on the Plateau. With the improved BIOME4 model, possible changes in the vegetation distribution were simulated under climate change scenarios. The simulated results suggest that alpine meadows, steppes, and alpine sparse/cushion vegetation and deserts would shrink, while shrubs, broad-leaved forests, coniferous-broad-leaved mixed forests, and coniferous forests would expand. Among these types, shrubs, alpine meadows, and steppes would change the most. The shrubs vegetation would expand toward the northwest, replacing most alpine meadows and part of steppes, and thus causing their shrinkages. Yet broad-leaved forests and coniferous-broad-leaved mixed forests demonstrated smaller changes in their distributions. For all the forest types, the area of coniferous forests would increase the most by spreading to the interior of the Plateau.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vegetation distribution</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">BIOME4 model</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tibetan Plateau</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Responses of vegetation to climate change</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vegetation distribution</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wu, Shaohong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yin, Yunhe</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yin, Zhi-Yong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Regional Environmental Change</subfield><subfield code="d">Springer-Verlag, 2001</subfield><subfield code="g">11(2011), 4 vom: 10. Mai, Seite 905-915</subfield><subfield code="w">(DE-627)SPR008808457</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:11</subfield><subfield code="g">year:2011</subfield><subfield code="g">number:4</subfield><subfield code="g">day:10</subfield><subfield code="g">month:05</subfield><subfield code="g">pages:905-915</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s10113-011-0228-7</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</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_SPRINGER</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">11</subfield><subfield code="j">2011</subfield><subfield code="e">4</subfield><subfield code="b">10</subfield><subfield code="c">05</subfield><subfield code="h">905-915</subfield></datafield></record></collection>
|
| score |
7.401348 |