Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band
<p<Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at <span class="inline-form...
Ausführliche Beschreibung
Autor*in: |
L. Wu [verfasserIn] O. Hasekamp [verfasserIn] H. Hu [verfasserIn] J. aan de Brugh [verfasserIn] J. Landgraf [verfasserIn] A. Butz [verfasserIn] I. Aben [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2019 |
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Übergeordnetes Werk: |
In: Atmospheric Measurement Techniques - Copernicus Publications, 2009, 12(2019), Seite 6049-6058 |
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Übergeordnetes Werk: |
volume:12 ; year:2019 ; pages:6049-6058 |
Links: |
Link aufrufen |
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DOI / URN: |
10.5194/amt-12-6049-2019 |
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Katalog-ID: |
DOAJ029650119 |
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520 | |a <p<Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at <span class="inline-formula"<0.76</span< <span class="inline-formula"<µ</span<m and the weak and strong <span class="inline-formula"<CO<sub<2</sub<</span< absorption bands at <span class="inline-formula"<1.61</span< and <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m, respectively, to infer information on light scattering and the carbon dioxide column-averaged dry-air mole fraction <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span<. In this study, we propose a one-band <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrieval technique which uses only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band measurements from the Orbiting Carbon Observatory-2 (OCO-2) satellite. We examine the data quality by comparing the OCO-2 <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< with collocated ground-based measurements from the Total Carbon Column Observing Network (TCCON). Over land and ocean the OCO-2 one-band retrieval shows differences from TCCON observations with a standard deviation of <span class="inline-formula"<∼1.30</span< ppm and a station-to-station variability of <span class="inline-formula"<∼0.50</span< ppm. Moreover, we compare one-band and three-band retrievals over Europe, the Middle East, and Africa and see high correlation between the two retrievals with a SD of <span class="inline-formula"<0.93</span< ppm. Compared to the three-band retrievals, <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrievals using only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band have similar retrieval accuracy, precision, and data yield.</p< | ||
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700 | 0 | |a J. Landgraf |e verfasserin |4 aut | |
700 | 0 | |a A. Butz |e verfasserin |4 aut | |
700 | 0 | |a I. Aben |e verfasserin |4 aut | |
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10.5194/amt-12-6049-2019 doi (DE-627)DOAJ029650119 (DE-599)DOAJ635772ef94314aa6bb9f806e4ceb21fe DE-627 ger DE-627 rakwb eng TA170-171 TA715-787 L. Wu verfasserin aut Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at <span class="inline-formula"<0.76</span< <span class="inline-formula"<µ</span<m and the weak and strong <span class="inline-formula"<CO<sub<2</sub<</span< absorption bands at <span class="inline-formula"<1.61</span< and <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m, respectively, to infer information on light scattering and the carbon dioxide column-averaged dry-air mole fraction <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span<. In this study, we propose a one-band <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrieval technique which uses only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band measurements from the Orbiting Carbon Observatory-2 (OCO-2) satellite. We examine the data quality by comparing the OCO-2 <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< with collocated ground-based measurements from the Total Carbon Column Observing Network (TCCON). Over land and ocean the OCO-2 one-band retrieval shows differences from TCCON observations with a standard deviation of <span class="inline-formula"<∼1.30</span< ppm and a station-to-station variability of <span class="inline-formula"<∼0.50</span< ppm. Moreover, we compare one-band and three-band retrievals over Europe, the Middle East, and Africa and see high correlation between the two retrievals with a SD of <span class="inline-formula"<0.93</span< ppm. Compared to the three-band retrievals, <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrievals using only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band have similar retrieval accuracy, precision, and data yield.</p< Environmental engineering Earthwork. Foundations O. Hasekamp verfasserin aut H. Hu verfasserin aut J. aan de Brugh verfasserin aut J. Landgraf verfasserin aut A. Butz verfasserin aut I. Aben verfasserin aut In Atmospheric Measurement Techniques Copernicus Publications, 2009 12(2019), Seite 6049-6058 (DE-627)605214441 (DE-600)2505596-3 18678548 nnns volume:12 year:2019 pages:6049-6058 https://doi.org/10.5194/amt-12-6049-2019 kostenfrei https://doaj.org/article/635772ef94314aa6bb9f806e4ceb21fe kostenfrei https://www.atmos-meas-tech.net/12/6049/2019/amt-12-6049-2019.pdf kostenfrei https://doaj.org/toc/1867-1381 Journal toc kostenfrei https://doaj.org/toc/1867-8548 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA 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_2111 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 12 2019 6049-6058 |
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10.5194/amt-12-6049-2019 doi (DE-627)DOAJ029650119 (DE-599)DOAJ635772ef94314aa6bb9f806e4ceb21fe DE-627 ger DE-627 rakwb eng TA170-171 TA715-787 L. Wu verfasserin aut Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at <span class="inline-formula"<0.76</span< <span class="inline-formula"<µ</span<m and the weak and strong <span class="inline-formula"<CO<sub<2</sub<</span< absorption bands at <span class="inline-formula"<1.61</span< and <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m, respectively, to infer information on light scattering and the carbon dioxide column-averaged dry-air mole fraction <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span<. In this study, we propose a one-band <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrieval technique which uses only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band measurements from the Orbiting Carbon Observatory-2 (OCO-2) satellite. We examine the data quality by comparing the OCO-2 <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< with collocated ground-based measurements from the Total Carbon Column Observing Network (TCCON). Over land and ocean the OCO-2 one-band retrieval shows differences from TCCON observations with a standard deviation of <span class="inline-formula"<∼1.30</span< ppm and a station-to-station variability of <span class="inline-formula"<∼0.50</span< ppm. Moreover, we compare one-band and three-band retrievals over Europe, the Middle East, and Africa and see high correlation between the two retrievals with a SD of <span class="inline-formula"<0.93</span< ppm. Compared to the three-band retrievals, <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrievals using only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band have similar retrieval accuracy, precision, and data yield.</p< Environmental engineering Earthwork. Foundations O. Hasekamp verfasserin aut H. Hu verfasserin aut J. aan de Brugh verfasserin aut J. Landgraf verfasserin aut A. Butz verfasserin aut I. Aben verfasserin aut In Atmospheric Measurement Techniques Copernicus Publications, 2009 12(2019), Seite 6049-6058 (DE-627)605214441 (DE-600)2505596-3 18678548 nnns volume:12 year:2019 pages:6049-6058 https://doi.org/10.5194/amt-12-6049-2019 kostenfrei https://doaj.org/article/635772ef94314aa6bb9f806e4ceb21fe kostenfrei https://www.atmos-meas-tech.net/12/6049/2019/amt-12-6049-2019.pdf kostenfrei https://doaj.org/toc/1867-1381 Journal toc kostenfrei https://doaj.org/toc/1867-8548 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA 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_2111 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 12 2019 6049-6058 |
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10.5194/amt-12-6049-2019 doi (DE-627)DOAJ029650119 (DE-599)DOAJ635772ef94314aa6bb9f806e4ceb21fe DE-627 ger DE-627 rakwb eng TA170-171 TA715-787 L. Wu verfasserin aut Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at <span class="inline-formula"<0.76</span< <span class="inline-formula"<µ</span<m and the weak and strong <span class="inline-formula"<CO<sub<2</sub<</span< absorption bands at <span class="inline-formula"<1.61</span< and <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m, respectively, to infer information on light scattering and the carbon dioxide column-averaged dry-air mole fraction <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span<. In this study, we propose a one-band <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrieval technique which uses only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band measurements from the Orbiting Carbon Observatory-2 (OCO-2) satellite. We examine the data quality by comparing the OCO-2 <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< with collocated ground-based measurements from the Total Carbon Column Observing Network (TCCON). Over land and ocean the OCO-2 one-band retrieval shows differences from TCCON observations with a standard deviation of <span class="inline-formula"<∼1.30</span< ppm and a station-to-station variability of <span class="inline-formula"<∼0.50</span< ppm. Moreover, we compare one-band and three-band retrievals over Europe, the Middle East, and Africa and see high correlation between the two retrievals with a SD of <span class="inline-formula"<0.93</span< ppm. Compared to the three-band retrievals, <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrievals using only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band have similar retrieval accuracy, precision, and data yield.</p< Environmental engineering Earthwork. Foundations O. Hasekamp verfasserin aut H. Hu verfasserin aut J. aan de Brugh verfasserin aut J. Landgraf verfasserin aut A. Butz verfasserin aut I. Aben verfasserin aut In Atmospheric Measurement Techniques Copernicus Publications, 2009 12(2019), Seite 6049-6058 (DE-627)605214441 (DE-600)2505596-3 18678548 nnns volume:12 year:2019 pages:6049-6058 https://doi.org/10.5194/amt-12-6049-2019 kostenfrei https://doaj.org/article/635772ef94314aa6bb9f806e4ceb21fe kostenfrei https://www.atmos-meas-tech.net/12/6049/2019/amt-12-6049-2019.pdf kostenfrei https://doaj.org/toc/1867-1381 Journal toc kostenfrei https://doaj.org/toc/1867-8548 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA 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_2111 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 12 2019 6049-6058 |
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10.5194/amt-12-6049-2019 doi (DE-627)DOAJ029650119 (DE-599)DOAJ635772ef94314aa6bb9f806e4ceb21fe DE-627 ger DE-627 rakwb eng TA170-171 TA715-787 L. Wu verfasserin aut Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at <span class="inline-formula"<0.76</span< <span class="inline-formula"<µ</span<m and the weak and strong <span class="inline-formula"<CO<sub<2</sub<</span< absorption bands at <span class="inline-formula"<1.61</span< and <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m, respectively, to infer information on light scattering and the carbon dioxide column-averaged dry-air mole fraction <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span<. In this study, we propose a one-band <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrieval technique which uses only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band measurements from the Orbiting Carbon Observatory-2 (OCO-2) satellite. We examine the data quality by comparing the OCO-2 <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< with collocated ground-based measurements from the Total Carbon Column Observing Network (TCCON). Over land and ocean the OCO-2 one-band retrieval shows differences from TCCON observations with a standard deviation of <span class="inline-formula"<∼1.30</span< ppm and a station-to-station variability of <span class="inline-formula"<∼0.50</span< ppm. Moreover, we compare one-band and three-band retrievals over Europe, the Middle East, and Africa and see high correlation between the two retrievals with a SD of <span class="inline-formula"<0.93</span< ppm. Compared to the three-band retrievals, <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrievals using only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band have similar retrieval accuracy, precision, and data yield.</p< Environmental engineering Earthwork. Foundations O. Hasekamp verfasserin aut H. Hu verfasserin aut J. aan de Brugh verfasserin aut J. Landgraf verfasserin aut A. Butz verfasserin aut I. Aben verfasserin aut In Atmospheric Measurement Techniques Copernicus Publications, 2009 12(2019), Seite 6049-6058 (DE-627)605214441 (DE-600)2505596-3 18678548 nnns volume:12 year:2019 pages:6049-6058 https://doi.org/10.5194/amt-12-6049-2019 kostenfrei https://doaj.org/article/635772ef94314aa6bb9f806e4ceb21fe kostenfrei https://www.atmos-meas-tech.net/12/6049/2019/amt-12-6049-2019.pdf kostenfrei https://doaj.org/toc/1867-1381 Journal toc kostenfrei https://doaj.org/toc/1867-8548 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA 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_2111 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 12 2019 6049-6058 |
allfieldsSound |
10.5194/amt-12-6049-2019 doi (DE-627)DOAJ029650119 (DE-599)DOAJ635772ef94314aa6bb9f806e4ceb21fe DE-627 ger DE-627 rakwb eng TA170-171 TA715-787 L. Wu verfasserin aut Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at <span class="inline-formula"<0.76</span< <span class="inline-formula"<µ</span<m and the weak and strong <span class="inline-formula"<CO<sub<2</sub<</span< absorption bands at <span class="inline-formula"<1.61</span< and <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m, respectively, to infer information on light scattering and the carbon dioxide column-averaged dry-air mole fraction <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span<. In this study, we propose a one-band <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrieval technique which uses only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band measurements from the Orbiting Carbon Observatory-2 (OCO-2) satellite. We examine the data quality by comparing the OCO-2 <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< with collocated ground-based measurements from the Total Carbon Column Observing Network (TCCON). Over land and ocean the OCO-2 one-band retrieval shows differences from TCCON observations with a standard deviation of <span class="inline-formula"<∼1.30</span< ppm and a station-to-station variability of <span class="inline-formula"<∼0.50</span< ppm. Moreover, we compare one-band and three-band retrievals over Europe, the Middle East, and Africa and see high correlation between the two retrievals with a SD of <span class="inline-formula"<0.93</span< ppm. Compared to the three-band retrievals, <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrievals using only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band have similar retrieval accuracy, precision, and data yield.</p< Environmental engineering Earthwork. Foundations O. Hasekamp verfasserin aut H. Hu verfasserin aut J. aan de Brugh verfasserin aut J. Landgraf verfasserin aut A. Butz verfasserin aut I. Aben verfasserin aut In Atmospheric Measurement Techniques Copernicus Publications, 2009 12(2019), Seite 6049-6058 (DE-627)605214441 (DE-600)2505596-3 18678548 nnns volume:12 year:2019 pages:6049-6058 https://doi.org/10.5194/amt-12-6049-2019 kostenfrei https://doaj.org/article/635772ef94314aa6bb9f806e4ceb21fe kostenfrei https://www.atmos-meas-tech.net/12/6049/2019/amt-12-6049-2019.pdf kostenfrei https://doaj.org/toc/1867-1381 Journal toc kostenfrei https://doaj.org/toc/1867-8548 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA 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_2111 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 12 2019 6049-6058 |
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Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band |
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full-physics carbon dioxide retrievals from the orbiting carbon observatory-2 (oco-2) satellite by only using the 2.06 µm band |
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Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band |
abstract |
<p<Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at <span class="inline-formula"<0.76</span< <span class="inline-formula"<µ</span<m and the weak and strong <span class="inline-formula"<CO<sub<2</sub<</span< absorption bands at <span class="inline-formula"<1.61</span< and <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m, respectively, to infer information on light scattering and the carbon dioxide column-averaged dry-air mole fraction <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span<. In this study, we propose a one-band <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrieval technique which uses only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band measurements from the Orbiting Carbon Observatory-2 (OCO-2) satellite. We examine the data quality by comparing the OCO-2 <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< with collocated ground-based measurements from the Total Carbon Column Observing Network (TCCON). Over land and ocean the OCO-2 one-band retrieval shows differences from TCCON observations with a standard deviation of <span class="inline-formula"<∼1.30</span< ppm and a station-to-station variability of <span class="inline-formula"<∼0.50</span< ppm. Moreover, we compare one-band and three-band retrievals over Europe, the Middle East, and Africa and see high correlation between the two retrievals with a SD of <span class="inline-formula"<0.93</span< ppm. Compared to the three-band retrievals, <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrievals using only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band have similar retrieval accuracy, precision, and data yield.</p< |
abstractGer |
<p<Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at <span class="inline-formula"<0.76</span< <span class="inline-formula"<µ</span<m and the weak and strong <span class="inline-formula"<CO<sub<2</sub<</span< absorption bands at <span class="inline-formula"<1.61</span< and <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m, respectively, to infer information on light scattering and the carbon dioxide column-averaged dry-air mole fraction <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span<. In this study, we propose a one-band <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrieval technique which uses only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band measurements from the Orbiting Carbon Observatory-2 (OCO-2) satellite. We examine the data quality by comparing the OCO-2 <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< with collocated ground-based measurements from the Total Carbon Column Observing Network (TCCON). Over land and ocean the OCO-2 one-band retrieval shows differences from TCCON observations with a standard deviation of <span class="inline-formula"<∼1.30</span< ppm and a station-to-station variability of <span class="inline-formula"<∼0.50</span< ppm. Moreover, we compare one-band and three-band retrievals over Europe, the Middle East, and Africa and see high correlation between the two retrievals with a SD of <span class="inline-formula"<0.93</span< ppm. Compared to the three-band retrievals, <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrievals using only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band have similar retrieval accuracy, precision, and data yield.</p< |
abstract_unstemmed |
<p<Passive remote sensing of atmospheric carbon dioxide uses spectroscopic measurements of sunlight backscattered by the Earth's surface and atmosphere. The current state-of-the-art retrieval methods use three different spectral bands, the oxygen A band at <span class="inline-formula"<0.76</span< <span class="inline-formula"<µ</span<m and the weak and strong <span class="inline-formula"<CO<sub<2</sub<</span< absorption bands at <span class="inline-formula"<1.61</span< and <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m, respectively, to infer information on light scattering and the carbon dioxide column-averaged dry-air mole fraction <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span<. In this study, we propose a one-band <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrieval technique which uses only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band measurements from the Orbiting Carbon Observatory-2 (OCO-2) satellite. We examine the data quality by comparing the OCO-2 <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< with collocated ground-based measurements from the Total Carbon Column Observing Network (TCCON). Over land and ocean the OCO-2 one-band retrieval shows differences from TCCON observations with a standard deviation of <span class="inline-formula"<∼1.30</span< ppm and a station-to-station variability of <span class="inline-formula"<∼0.50</span< ppm. Moreover, we compare one-band and three-band retrievals over Europe, the Middle East, and Africa and see high correlation between the two retrievals with a SD of <span class="inline-formula"<0.93</span< ppm. Compared to the three-band retrievals, <span class="inline-formula"<<i<X</i<CO<sub<2</sub<</span< retrievals using only the <span class="inline-formula"<2.06</span< <span class="inline-formula"<µ</span<m band have similar retrieval accuracy, precision, and data yield.</p< |
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Full-physics carbon dioxide retrievals from the Orbiting Carbon Observatory-2 (OCO-2) satellite by only using the 2.06 µm band |
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https://doi.org/10.5194/amt-12-6049-2019 https://doaj.org/article/635772ef94314aa6bb9f806e4ceb21fe https://www.atmos-meas-tech.net/12/6049/2019/amt-12-6049-2019.pdf https://doaj.org/toc/1867-1381 https://doaj.org/toc/1867-8548 |
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