Improved water vapour retrieval from AMSU-B and MHS in the Arctic

Monitoring of water vapour in the Arctic on long timescales is essential for predicting Arctic weather and understanding climate trends, as well as addressing its influence on the positive feedback loop contributing to Arctic amplification. However, this is challenged by the sparseness of in situ me...

Full description

Bibliographic Details
Published in:Atmospheric Measurement Techniques
Main Authors: Arantxa M. Triana-Gómez, Georg Heygster, Christian Melsheimer, Gunnar Spreen, NEGUSINI, MONIA, Boyan H. Petkov
Other Authors: ITA, DEU
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://hdl.handle.net/20.500.12386/31364
https://doi.org/10.5194/amt-13-3697-2020
https://amt.copernicus.org/articles/13/3697/2020/
_version_ 1835010551805116416
author Arantxa M. Triana-Gómez
Georg Heygster
Christian Melsheimer
Gunnar Spreen
NEGUSINI, MONIA
Boyan H. Petkov
author2 ITA
DEU
author_facet Arantxa M. Triana-Gómez
Georg Heygster
Christian Melsheimer
Gunnar Spreen
NEGUSINI, MONIA
Boyan H. Petkov
author_sort Arantxa M. Triana-Gómez
collection Unknown
container_issue 7
container_start_page 3697
container_title Atmospheric Measurement Techniques
container_volume 13
description Monitoring of water vapour in the Arctic on long timescales is essential for predicting Arctic weather and understanding climate trends, as well as addressing its influence on the positive feedback loop contributing to Arctic amplification. However, this is challenged by the sparseness of in situ measurements and the problems that standard remote sensing retrieval methods for water vapour have in Arctic conditions. Here, we present advances in a retrieval algorithm for vertically integrated water vapour (total water vapour, TWV) in polar regions from data of satellite-based microwave humidity sounders: (1) in addition to AMSU-B (Advanced Microwave Sounding Unit-B), we can now also use data from the successor instrument MHS (Microwave Humidity Sounder), and (2) artefacts caused by high cloud ice content in convective clouds are filtered out. Comparison to in situ measurements using GPS and radiosondes during 2008 and 2009, as well as to radiosondes during the NICE2015 campaign and to ERA5 reanalysis, show the overall good performance of the updated algorithm.
format Article in Journal/Newspaper
genre Arctic
genre_facet Arctic
geographic Arctic
geographic_facet Arctic
id ftinstnastrofisi:oai:openaccess.inaf.it:20.500.12386/31364
institution Open Polar
language English
op_collection_id ftinstnastrofisi
op_container_end_page 3715
op_doi https://doi.org/20.500.12386/3136410.5194/amt-13-3697-2020
op_relation ATMOSPHERIC MEASUREMENT TECHNIQUES
http://hdl.handle.net/20.500.12386/31364
WOS:000550596600002
https://amt.copernicus.org/articles/13/3697/2020/
2020AMT.13.3697
op_rights open
publishDate 2020
record_format openpolar
spelling ftinstnastrofisi:oai:openaccess.inaf.it:20.500.12386/31364 2025-06-15T14:18:27+00:00 Improved water vapour retrieval from AMSU-B and MHS in the Arctic Arantxa M. Triana-Gómez Georg Heygster Christian Melsheimer Gunnar Spreen NEGUSINI, MONIA Boyan H. Petkov ITA DEU 2020 https://hdl.handle.net/20.500.12386/31364 https://doi.org/10.5194/amt-13-3697-2020 https://amt.copernicus.org/articles/13/3697/2020/ en eng ATMOSPHERIC MEASUREMENT TECHNIQUES http://hdl.handle.net/20.500.12386/31364 WOS:000550596600002 https://amt.copernicus.org/articles/13/3697/2020/ 2020AMT.13.3697 open Article 2020 ftinstnastrofisi https://doi.org/20.500.12386/3136410.5194/amt-13-3697-2020 2025-05-16T03:20:39Z Monitoring of water vapour in the Arctic on long timescales is essential for predicting Arctic weather and understanding climate trends, as well as addressing its influence on the positive feedback loop contributing to Arctic amplification. However, this is challenged by the sparseness of in situ measurements and the problems that standard remote sensing retrieval methods for water vapour have in Arctic conditions. Here, we present advances in a retrieval algorithm for vertically integrated water vapour (total water vapour, TWV) in polar regions from data of satellite-based microwave humidity sounders: (1) in addition to AMSU-B (Advanced Microwave Sounding Unit-B), we can now also use data from the successor instrument MHS (Microwave Humidity Sounder), and (2) artefacts caused by high cloud ice content in convective clouds are filtered out. Comparison to in situ measurements using GPS and radiosondes during 2008 and 2009, as well as to radiosondes during the NICE2015 campaign and to ERA5 reanalysis, show the overall good performance of the updated algorithm. Article in Journal/Newspaper Arctic Unknown Arctic Atmospheric Measurement Techniques 13 7 3697 3715
spellingShingle Arantxa M. Triana-Gómez
Georg Heygster
Christian Melsheimer
Gunnar Spreen
NEGUSINI, MONIA
Boyan H. Petkov
Improved water vapour retrieval from AMSU-B and MHS in the Arctic
title Improved water vapour retrieval from AMSU-B and MHS in the Arctic
title_full Improved water vapour retrieval from AMSU-B and MHS in the Arctic
title_fullStr Improved water vapour retrieval from AMSU-B and MHS in the Arctic
title_full_unstemmed Improved water vapour retrieval from AMSU-B and MHS in the Arctic
title_short Improved water vapour retrieval from AMSU-B and MHS in the Arctic
title_sort improved water vapour retrieval from amsu-b and mhs in the arctic
url https://hdl.handle.net/20.500.12386/31364
https://doi.org/10.5194/amt-13-3697-2020
https://amt.copernicus.org/articles/13/3697/2020/