A Direct Comparison of Passive Polarimetry and Scatterometry Under Low- and High-Wind Conditions
The University of Massachusetts Microwave Remote Sensing Laboratory (MIRSL) gathered coincident active and passive measurements of the ocean surface from the NASA Wallops P3 during the Ocean Wind Imaging (OWI) Experiment. The experiment consisted of five missions flown over the Labrador Sea. Surface...
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ftdtic:ADA336859 2023-05-15T17:06:06+02:00 A Direct Comparison of Passive Polarimetry and Scatterometry Under Low- and High-Wind Conditions Swift, Calvin T. Carswell, James R. MASSACHUSETTS UNIV AMHERST MICROWAVE REMOTE SENSING LAB 1997-12-31 text/html http://www.dtic.mil/docs/citations/ADA336859 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA336859 en eng http://www.dtic.mil/docs/citations/ADA336859 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Meteorology Test Facilities Equipment and Methods *RADIOMETERS *MARINE METEOROLOGY *SCATTEROMETERS OCEAN SURFACE PASSIVE SYSTEMS POLARIMETRY BACKSCATTERING WIND DIRECTION WIND VELOCITY C BAND LABRADOR SEA *OCEAN WINDS C-BAND SCATTEROMETERS KA-BAND RADIOMETERS Text 1997 ftdtic 2016-02-19T21:43:37Z The University of Massachusetts Microwave Remote Sensing Laboratory (MIRSL) gathered coincident active and passive measurements of the ocean surface from the NASA Wallops P3 during the Ocean Wind Imaging (OWI) Experiment. The experiment consisted of five missions flown over the Labrador Sea. Surface winds from 8 to 16 m/s were sampled, and approximately thirty hours of data were collected. The passive measurements were obtained with a novel Ka-band conically scanning passive polarimeter (KASPR) that simultaneously measures the four brightness temperature Stokes parameters by using a correlation receiver. The active measurements were collected by a conically scanning C-band scatterometer (CSCAT) that simultaneously measures the backscatter at four separate incidence angles. Analysis of the passive data shows a wind directional signature in the vertically and horizontally polarized brightness temperature measurements at the high winds. For vertical polarization, the wind direction signature is best described by a two-term Fourier cosine series, while for horizontal polarization, the wind direction signature is described by a three-term Fourier cosine series. This report presents these results as well as summarizes the data obtained and the future analysis plans. Text Labrador Sea Defense Technical Information Center: DTIC Technical Reports database |
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Defense Technical Information Center: DTIC Technical Reports database |
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language |
English |
topic |
Meteorology Test Facilities Equipment and Methods *RADIOMETERS *MARINE METEOROLOGY *SCATTEROMETERS OCEAN SURFACE PASSIVE SYSTEMS POLARIMETRY BACKSCATTERING WIND DIRECTION WIND VELOCITY C BAND LABRADOR SEA *OCEAN WINDS C-BAND SCATTEROMETERS KA-BAND RADIOMETERS |
spellingShingle |
Meteorology Test Facilities Equipment and Methods *RADIOMETERS *MARINE METEOROLOGY *SCATTEROMETERS OCEAN SURFACE PASSIVE SYSTEMS POLARIMETRY BACKSCATTERING WIND DIRECTION WIND VELOCITY C BAND LABRADOR SEA *OCEAN WINDS C-BAND SCATTEROMETERS KA-BAND RADIOMETERS Swift, Calvin T. Carswell, James R. A Direct Comparison of Passive Polarimetry and Scatterometry Under Low- and High-Wind Conditions |
topic_facet |
Meteorology Test Facilities Equipment and Methods *RADIOMETERS *MARINE METEOROLOGY *SCATTEROMETERS OCEAN SURFACE PASSIVE SYSTEMS POLARIMETRY BACKSCATTERING WIND DIRECTION WIND VELOCITY C BAND LABRADOR SEA *OCEAN WINDS C-BAND SCATTEROMETERS KA-BAND RADIOMETERS |
description |
The University of Massachusetts Microwave Remote Sensing Laboratory (MIRSL) gathered coincident active and passive measurements of the ocean surface from the NASA Wallops P3 during the Ocean Wind Imaging (OWI) Experiment. The experiment consisted of five missions flown over the Labrador Sea. Surface winds from 8 to 16 m/s were sampled, and approximately thirty hours of data were collected. The passive measurements were obtained with a novel Ka-band conically scanning passive polarimeter (KASPR) that simultaneously measures the four brightness temperature Stokes parameters by using a correlation receiver. The active measurements were collected by a conically scanning C-band scatterometer (CSCAT) that simultaneously measures the backscatter at four separate incidence angles. Analysis of the passive data shows a wind directional signature in the vertically and horizontally polarized brightness temperature measurements at the high winds. For vertical polarization, the wind direction signature is best described by a two-term Fourier cosine series, while for horizontal polarization, the wind direction signature is described by a three-term Fourier cosine series. This report presents these results as well as summarizes the data obtained and the future analysis plans. |
author2 |
MASSACHUSETTS UNIV AMHERST MICROWAVE REMOTE SENSING LAB |
format |
Text |
author |
Swift, Calvin T. Carswell, James R. |
author_facet |
Swift, Calvin T. Carswell, James R. |
author_sort |
Swift, Calvin T. |
title |
A Direct Comparison of Passive Polarimetry and Scatterometry Under Low- and High-Wind Conditions |
title_short |
A Direct Comparison of Passive Polarimetry and Scatterometry Under Low- and High-Wind Conditions |
title_full |
A Direct Comparison of Passive Polarimetry and Scatterometry Under Low- and High-Wind Conditions |
title_fullStr |
A Direct Comparison of Passive Polarimetry and Scatterometry Under Low- and High-Wind Conditions |
title_full_unstemmed |
A Direct Comparison of Passive Polarimetry and Scatterometry Under Low- and High-Wind Conditions |
title_sort |
direct comparison of passive polarimetry and scatterometry under low- and high-wind conditions |
publishDate |
1997 |
url |
http://www.dtic.mil/docs/citations/ADA336859 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA336859 |
genre |
Labrador Sea |
genre_facet |
Labrador Sea |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA336859 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766061080896864256 |