Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2018)

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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Bibliographic Details
Main Authors: Nomokonova, Tatiana, Ritter, Christoph, Ebell, Kerstin
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
AC3
RS
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.902099
https://doi.org/10.1594/PANGAEA.902099
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.902099
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.902099 2024-09-15T18:27:19+00:00 Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2018) Nomokonova, Tatiana Ritter, Christoph Ebell, Kerstin LATITUDE: 78.920000 * LONGITUDE: 11.930000 * DATE/TIME START: 2018-01-01T00:00:00 * DATE/TIME END: 2018-12-31T00:00:00 * MINIMUM ELEVATION: 11.0 m * MAXIMUM ELEVATION: 11.0 m 2019 text/tab-separated-values, 1408 data points https://doi.pangaea.de/10.1594/PANGAEA.902099 https://doi.org/10.1594/PANGAEA.902099 en eng PANGAEA https://doi.org/10.1594/PANGAEA.902183 https://doi.pangaea.de/10.1594/PANGAEA.902099 https://doi.org/10.1594/PANGAEA.902099 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess 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.90209910.1594/PANGAEA.902183 2024-07-24T02:31:42Z 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 Ny Ålesund Ny-Ålesund Svalbard Spitsbergen PANGAEA - Data Publisher for Earth & Environmental Science 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 (2018)
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 (2018)
title_short Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2018)
title_full Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2018)
title_fullStr Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2018)
title_full_unstemmed Liquid water path of HATPRO microwave radiometer at AWIPEV, Ny-Ålesund (2018)
title_sort liquid water path of hatpro microwave radiometer at awipev, ny-ålesund (2018)
publisher PANGAEA
publishDate 2019
url https://doi.pangaea.de/10.1594/PANGAEA.902099
https://doi.org/10.1594/PANGAEA.902099
op_coverage LATITUDE: 78.920000 * LONGITUDE: 11.930000 * DATE/TIME START: 2018-01-01T00:00:00 * DATE/TIME END: 2018-12-31T00:00:00 * MINIMUM ELEVATION: 11.0 m * MAXIMUM ELEVATION: 11.0 m
long_lat ENVELOPE(11.930000,11.930000,78.920000,78.920000)
genre Ny Ålesund
Ny-Ålesund
Svalbard
Spitsbergen
genre_facet Ny Ålesund
Ny-Ålesund
Svalbard
Spitsbergen
op_relation https://doi.org/10.1594/PANGAEA.902183
https://doi.pangaea.de/10.1594/PANGAEA.902099
https://doi.org/10.1594/PANGAEA.902099
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.90209910.1594/PANGAEA.902183
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