Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2016)
The microwave radiometer HATPRO has seven K band (22.235-31.4 GHz) channels that are sensitive to the path integrated amount of cloud liquid water (clwvi) and the path integrated amount of water vapor (precipitable water, prw). These files contain clwvi as a function of measurement time, elevation a...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.902096 2023-05-15T15:06:31+02:00 Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2016) Nomokonova, Tatiana Ritter, Christoph Ebell, Kerstin LATITUDE: 78.920000 * LONGITUDE: 11.930000 * DATE/TIME START: 2016-05-01T00:00:00 * DATE/TIME END: 2016-12-31T00:00:00 * MINIMUM ELEVATION: 11.0 m * MAXIMUM ELEVATION: 11.0 m 2019-05-27 text/tab-separated-values, 972 data points https://doi.pangaea.de/10.1594/PANGAEA.902096 https://doi.org/10.1594/PANGAEA.902096 en eng PANGAEA https://doi.org/10.1594/PANGAEA.902183 https://doi.pangaea.de/10.1594/PANGAEA.902096 https://doi.org/10.1594/PANGAEA.902096 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY AC3 Arctic Amplification AWIPEV AWIPEV_based clouds DATE/TIME File format File name File size Koldewey liquid water path microwave radiometer Research station RS Spitsbergen Svalbard Uniform resource locator/link to file Dataset 2019 ftpangaea https://doi.org/10.1594/PANGAEA.902096 https://doi.org/10.1594/PANGAEA.902183 2023-01-20T10:00:27Z The microwave radiometer HATPRO has seven K band (22.235-31.4 GHz) channels that are sensitive to the path integrated amount of cloud liquid water (clwvi) and the path integrated amount of water vapor (precipitable water, prw). These files contain clwvi as a function of measurement time, elevation and azimuth angle observing direction. clwvi is based on multi-variate regression retrievals (see also Crewell and Löhnert, 2003; doi:10.1029/2002RS002654). Provided uncertainties describe the expected standard error of clwvi. Note, that clwvi values are given for all available times so that it is up to the user to decide whether or not to use the values if quality flags are set. Additionally included are temperature, pressure and humidity at the instrument location as well quality flags characterizing the instrument and retrieval performance. Dataset Arctic Ny Ålesund Ny-Ålesund Svalbard Spitsbergen PANGAEA - Data Publisher for Earth & Environmental Science Arctic Svalbard Ny-Ålesund ENVELOPE(11.930000,11.930000,78.920000,78.920000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AC3 Arctic Amplification AWIPEV AWIPEV_based clouds DATE/TIME File format File name File size Koldewey liquid water path microwave radiometer Research station RS Spitsbergen Svalbard Uniform resource locator/link to file |
spellingShingle |
AC3 Arctic Amplification AWIPEV AWIPEV_based clouds DATE/TIME File format File name File size Koldewey liquid water path microwave radiometer Research station RS Spitsbergen Svalbard Uniform resource locator/link to file Nomokonova, Tatiana Ritter, Christoph Ebell, Kerstin Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2016) |
topic_facet |
AC3 Arctic Amplification AWIPEV AWIPEV_based clouds DATE/TIME File format File name File size Koldewey liquid water path microwave radiometer Research station RS Spitsbergen Svalbard Uniform resource locator/link to file |
description |
The microwave radiometer HATPRO has seven K band (22.235-31.4 GHz) channels that are sensitive to the path integrated amount of cloud liquid water (clwvi) and the path integrated amount of water vapor (precipitable water, prw). These files contain clwvi as a function of measurement time, elevation and azimuth angle observing direction. clwvi is based on multi-variate regression retrievals (see also Crewell and Löhnert, 2003; doi:10.1029/2002RS002654). Provided uncertainties describe the expected standard error of clwvi. Note, that clwvi values are given for all available times so that it is up to the user to decide whether or not to use the values if quality flags are set. Additionally included are temperature, pressure and humidity at the instrument location as well quality flags characterizing the instrument and retrieval performance. |
format |
Dataset |
author |
Nomokonova, Tatiana Ritter, Christoph Ebell, Kerstin |
author_facet |
Nomokonova, Tatiana Ritter, Christoph Ebell, Kerstin |
author_sort |
Nomokonova, Tatiana |
title |
Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2016) |
title_short |
Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2016) |
title_full |
Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2016) |
title_fullStr |
Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2016) |
title_full_unstemmed |
Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2016) |
title_sort |
liquid water path of hatpro microwave radiometer at awipev, ny-ålesund (2016) |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.902096 https://doi.org/10.1594/PANGAEA.902096 |
op_coverage |
LATITUDE: 78.920000 * LONGITUDE: 11.930000 * DATE/TIME START: 2016-05-01T00:00:00 * DATE/TIME END: 2016-12-31T00:00:00 * MINIMUM ELEVATION: 11.0 m * MAXIMUM ELEVATION: 11.0 m |
long_lat |
ENVELOPE(11.930000,11.930000,78.920000,78.920000) |
geographic |
Arctic Svalbard Ny-Ålesund |
geographic_facet |
Arctic Svalbard Ny-Ålesund |
genre |
Arctic Ny Ålesund Ny-Ålesund Svalbard Spitsbergen |
genre_facet |
Arctic Ny Ålesund Ny-Ålesund Svalbard Spitsbergen |
op_relation |
https://doi.org/10.1594/PANGAEA.902183 https://doi.pangaea.de/10.1594/PANGAEA.902096 https://doi.org/10.1594/PANGAEA.902096 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.902096 https://doi.org/10.1594/PANGAEA.902183 |
_version_ |
1766338109581033472 |