A Compact 183-GHz Radiometer for Water Vapor and Liquid Water Sensing
ProSensing Inc. has developed a G-band (183 GHz) water vapor radiometer (GVR) for long-term unattended measurements of low concentrations of atmospheric water vapor and liquid water. Precipitable water vapor (PWV) and liquid water path (LWP) are estimated from zenith brightness temperatures measured...
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Veröffentlicht in: | IEEE transactions on geoscience and remote sensing 2007-07, Vol.45 (7), p.2202-2206 |
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description | ProSensing Inc. has developed a G-band (183 GHz) water vapor radiometer (GVR) for long-term unattended measurements of low concentrations of atmospheric water vapor and liquid water. Precipitable water vapor (PWV) and liquid water path (LWP) are estimated from zenith brightness temperatures measured using four double-sideband receiver channels, which are centered at 183.31 1, 183.31 3, 183.31 7, and 183.31 14 GHz. A prototype ground-based version of the instrument was deployed at the Department of Energy Atmospheric Radiation Measurement program's North Slope of Alaska site near Barrow, AK, in April 2005, where it collected data continuously for one year. This paper presents design details, laboratory test results, and examples of retrieved PWV and LWP from measured brightness temperature data. |
doi_str_mv | 10.1109/TGRS.2006.888104 |
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Precipitable water vapor (PWV) and liquid water path (LWP) are estimated from zenith brightness temperatures measured using four double-sideband receiver channels, which are centered at 183.31 1, 183.31 3, 183.31 7, and 183.31 14 GHz. A prototype ground-based version of the instrument was deployed at the Department of Energy Atmospheric Radiation Measurement program's North Slope of Alaska site near Barrow, AK, in April 2005, where it collected data continuously for one year. 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Precipitable water vapor (PWV) and liquid water path (LWP) are estimated from zenith brightness temperatures measured using four double-sideband receiver channels, which are centered at 183.31 1, 183.31 3, 183.31 7, and 183.31 14 GHz. A prototype ground-based version of the instrument was deployed at the Department of Energy Atmospheric Radiation Measurement program's North Slope of Alaska site near Barrow, AK, in April 2005, where it collected data continuously for one year. This paper presents design details, laboratory test results, and examples of retrieved PWV and LWP from measured brightness temperature data.</description><subject>Applied geophysics</subject><subject>Atmospheric measurements</subject><subject>Atmospheric radiation</subject><subject>Brightness temperature</subject><subject>Channels</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Energy measurement</subject><subject>Exact sciences and technology</subject><subject>Information retrieval</subject><subject>Instruments</subject><subject>Internal geophysics</subject><subject>Laboratories</subject><subject>Liquids</subject><subject>Millimeter-wave radiometry</subject><subject>precipitable water vapor (PWV) and liquid water path (LWP) retrieval</subject><subject>Prototypes</subject><subject>Radiometers</subject><subject>Radiometry</subject><subject>Receivers</subject><subject>remote sensing</subject><subject>Temperature measurement</subject><subject>Testing</subject><subject>Water vapor</subject><subject>Zenith</subject><issn>0196-2892</issn><issn>1558-0644</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><sourceid>RIE</sourceid><recordid>eNp9kc1LAzEQxYMoWKt3wcsiiF62ZrLZfBxLqa1QENqqx5DdJLJlP9qke9C_3l1aFDx4msfM7z0YHkLXgEcAWD6uZ8vViGDMRkIIwPQEDSBNRYwZpadogEGymAhJztFFCBuMgabAB2g6jiZNtdX5PgKRxLP5V7TUpmgqu7c-co2P3nWv3vS207o20aLYtYU5rle2DkX9cYnOnC6DvTrOIXp9mq4n83jxMnuejBdxnoh0H1MwGcskkVbTjDimE2cocVxA7izF1EojDOQcQBumTUoyS2RmgBNCnaMmGaL7Q-7WN7vWhr2qipDbstS1bdqgBGeEcAJpRz78SwLnOGEJ4bxDb_-gm6b1dfeHEoxiKSSGDsIHKPdNCN46tfVFpf2nAqz6AlRfgOoLUIcCOsvdMVeHXJfO6zovwq9PCCkE76NvDlxhrf05U8IA8zT5Bh1ni_c</recordid><startdate>20070701</startdate><enddate>20070701</enddate><creator>Pazmany, A.L.</creator><general>IEEE</general><general>Institute of Electrical and Electronics Engineers</general><general>The Institute of Electrical and Electronics Engineers, Inc. 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Precipitable water vapor (PWV) and liquid water path (LWP) are estimated from zenith brightness temperatures measured using four double-sideband receiver channels, which are centered at 183.31 1, 183.31 3, 183.31 7, and 183.31 14 GHz. A prototype ground-based version of the instrument was deployed at the Department of Energy Atmospheric Radiation Measurement program's North Slope of Alaska site near Barrow, AK, in April 2005, where it collected data continuously for one year. This paper presents design details, laboratory test results, and examples of retrieved PWV and LWP from measured brightness temperature data.</abstract><cop>New York, NY</cop><pub>IEEE</pub><doi>10.1109/TGRS.2006.888104</doi><tpages>5</tpages></addata></record> |
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subjects | Applied geophysics Atmospheric measurements Atmospheric radiation Brightness temperature Channels Earth sciences Earth, ocean, space Energy measurement Exact sciences and technology Information retrieval Instruments Internal geophysics Laboratories Liquids Millimeter-wave radiometry precipitable water vapor (PWV) and liquid water path (LWP) retrieval Prototypes Radiometers Radiometry Receivers remote sensing Temperature measurement Testing Water vapor Zenith |
title | A Compact 183-GHz Radiometer for Water Vapor and Liquid Water Sensing |
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