HDO/H<sub>2</sub>O ratio retrievals from GOSAT

We report a new shortwave infrared (SWIR) retrieval of the column-averaged HDO/H<sub>2</sub>O ratio from the Japanese Greenhouse Gases Observing Satellite (GOSAT). From synthetic simulation studies, we have estimated that the inferred δD values will typically have random errors between 2...

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Main Authors: H. Boesch, N. M. Deutscher, T. Warneke, K. Byckling, A. J. Cogan, D. W. T. Griffith, J. Notholt, R. J. Parker, Z. Wang
Format: Article
Language:English
Published: Copernicus Publications 2013-03-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/6/599/2013/amt-6-599-2013.pdf
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spelling doaj-bb80109874ac4352ab9d76e16c91d6e62020-11-24T23:29:44ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482013-03-016359961210.5194/amt-6-599-2013HDO/H<sub>2</sub>O ratio retrievals from GOSATH. BoeschN. M. DeutscherT. WarnekeK. BycklingA. J. CoganD. W. T. GriffithJ. NotholtR. J. ParkerZ. WangWe report a new shortwave infrared (SWIR) retrieval of the column-averaged HDO/H<sub>2</sub>O ratio from the Japanese Greenhouse Gases Observing Satellite (GOSAT). From synthetic simulation studies, we have estimated that the inferred δD values will typically have random errors between 20&permil; (desert surface and 30° solar zenith angle) and 120&permil; (conifer surface and 60° solar zenith angle). We find that the retrieval will have a small but significant sensitivity to the presence of cirrus clouds, the HDO a priori profile shape and atmospheric temperature, which has the potential of introducing some regional-scale biases in the retrieval. From comparisons to ground-based column observations from the Total Carbon Column Observing Network (TCCON), we find differences between δD from GOSAT and TCCON of around −30&permil; for northern hemispheric sites which increase up to −70&permil; for Australian sites. The bias for the Australian sites significantly reduces when decreasing the spatial co-location criteria, which shows that spatial averaging contributes to the observed differences over Australia. The GOSAT retrievals allow mapping the global distribution of δD and its variations with season, and we find in our global GOSAT retrievals the expected strong latitudinal gradients with significant enhancements over the tropics. The comparisons to the ground-based TCCON network and the results of the global retrieval are very encouraging, and they show that δD retrieved from GOSAT should be a useful product that can be used to complement datasets from thermal-infrared sounder and ground-based networks and to extend the δD dataset from SWIR retrievals established from the recently ended SCIAMACHY mission.http://www.atmos-meas-tech.net/6/599/2013/amt-6-599-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author H. Boesch
N. M. Deutscher
T. Warneke
K. Byckling
A. J. Cogan
D. W. T. Griffith
J. Notholt
R. J. Parker
Z. Wang
spellingShingle H. Boesch
N. M. Deutscher
T. Warneke
K. Byckling
A. J. Cogan
D. W. T. Griffith
J. Notholt
R. J. Parker
Z. Wang
HDO/H<sub>2</sub>O ratio retrievals from GOSAT
Atmospheric Measurement Techniques
author_facet H. Boesch
N. M. Deutscher
T. Warneke
K. Byckling
A. J. Cogan
D. W. T. Griffith
J. Notholt
R. J. Parker
Z. Wang
author_sort H. Boesch
title HDO/H<sub>2</sub>O ratio retrievals from GOSAT
title_short HDO/H<sub>2</sub>O ratio retrievals from GOSAT
title_full HDO/H<sub>2</sub>O ratio retrievals from GOSAT
title_fullStr HDO/H<sub>2</sub>O ratio retrievals from GOSAT
title_full_unstemmed HDO/H<sub>2</sub>O ratio retrievals from GOSAT
title_sort hdo/h<sub>2</sub>o ratio retrievals from gosat
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2013-03-01
description We report a new shortwave infrared (SWIR) retrieval of the column-averaged HDO/H<sub>2</sub>O ratio from the Japanese Greenhouse Gases Observing Satellite (GOSAT). From synthetic simulation studies, we have estimated that the inferred δD values will typically have random errors between 20&permil; (desert surface and 30° solar zenith angle) and 120&permil; (conifer surface and 60° solar zenith angle). We find that the retrieval will have a small but significant sensitivity to the presence of cirrus clouds, the HDO a priori profile shape and atmospheric temperature, which has the potential of introducing some regional-scale biases in the retrieval. From comparisons to ground-based column observations from the Total Carbon Column Observing Network (TCCON), we find differences between δD from GOSAT and TCCON of around −30&permil; for northern hemispheric sites which increase up to −70&permil; for Australian sites. The bias for the Australian sites significantly reduces when decreasing the spatial co-location criteria, which shows that spatial averaging contributes to the observed differences over Australia. The GOSAT retrievals allow mapping the global distribution of δD and its variations with season, and we find in our global GOSAT retrievals the expected strong latitudinal gradients with significant enhancements over the tropics. The comparisons to the ground-based TCCON network and the results of the global retrieval are very encouraging, and they show that δD retrieved from GOSAT should be a useful product that can be used to complement datasets from thermal-infrared sounder and ground-based networks and to extend the δD dataset from SWIR retrievals established from the recently ended SCIAMACHY mission.
url http://www.atmos-meas-tech.net/6/599/2013/amt-6-599-2013.pdf
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