Analyzing Gaps in Hurricane Rain Coverage to Inform Future Satellite Proposals

This study assesses where tropical cyclone (TC) surface winds can be measured as a function of footprint sizes and wavelengths (Ka- Ku- and C-band). During TCs, most high-resolution surface observations are impeded by considerable ‘rain contamination.’ Under these conditions, high-resolution surface...

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Main Authors: Justin P. Stow, Mark A. Bourassa, Heather M. Holbach
Format: Article
Language:English
Published: MDPI AG 2020-08-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/17/2673
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spelling doaj-d6f1718d56a4442e8d40eeab334c6a2c2020-11-25T03:42:26ZengMDPI AGRemote Sensing2072-42922020-08-01122673267310.3390/rs12172673Analyzing Gaps in Hurricane Rain Coverage to Inform Future Satellite ProposalsJustin P. Stow0Mark A. Bourassa1Heather M. Holbach2Department of Earth, Ocean, and Atmospheric Sciences, Florida State University, Tallahassee, FL 32304, USADepartment of Earth, Ocean, and Atmospheric Sciences, Florida State University, Tallahassee, FL 32304, USADepartment of Earth, Ocean, and Atmospheric Sciences, Florida State University, Tallahassee, FL 32304, USAThis study assesses where tropical cyclone (TC) surface winds can be measured as a function of footprint sizes and wavelengths (Ka- Ku- and C-band). During TCs, most high-resolution surface observations are impeded by considerable ‘rain contamination.’ Under these conditions, high-resolution surface observations typically come from operational aircraft. Other techniques that provide high-resolution surface observations through rain are also hindered somewhat by rain contamination and are very sparse in space and time. The impacts of rain are functions of the remotely sensed wavelength and rain–drop size. Therefore, relative long wavelengths have been used to observe the surface, but at the cost of a larger footprint. We examine how smaller footprint sizes could be used to observe through gaps between moderate to heavy rainbands that circulate around the main low-pressure center of a TC. Aircraft data from the National Oceanic and Atmospheric Administration’s (NOAA’s) WP-3D turboprop aircraft will be used to create realistic maps of rain. Our results provide information on the satellite instrument characteristics needed to see the surface through these gaps. This information is expected to aid in developing hurricane-related applications of new higher-resolution satellites.https://www.mdpi.com/2072-4292/12/17/2673tropical cyclonerainband gapsatelliterain ratethresholdprecipitation
collection DOAJ
language English
format Article
sources DOAJ
author Justin P. Stow
Mark A. Bourassa
Heather M. Holbach
spellingShingle Justin P. Stow
Mark A. Bourassa
Heather M. Holbach
Analyzing Gaps in Hurricane Rain Coverage to Inform Future Satellite Proposals
Remote Sensing
tropical cyclone
rainband gap
satellite
rain rate
threshold
precipitation
author_facet Justin P. Stow
Mark A. Bourassa
Heather M. Holbach
author_sort Justin P. Stow
title Analyzing Gaps in Hurricane Rain Coverage to Inform Future Satellite Proposals
title_short Analyzing Gaps in Hurricane Rain Coverage to Inform Future Satellite Proposals
title_full Analyzing Gaps in Hurricane Rain Coverage to Inform Future Satellite Proposals
title_fullStr Analyzing Gaps in Hurricane Rain Coverage to Inform Future Satellite Proposals
title_full_unstemmed Analyzing Gaps in Hurricane Rain Coverage to Inform Future Satellite Proposals
title_sort analyzing gaps in hurricane rain coverage to inform future satellite proposals
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2020-08-01
description This study assesses where tropical cyclone (TC) surface winds can be measured as a function of footprint sizes and wavelengths (Ka- Ku- and C-band). During TCs, most high-resolution surface observations are impeded by considerable ‘rain contamination.’ Under these conditions, high-resolution surface observations typically come from operational aircraft. Other techniques that provide high-resolution surface observations through rain are also hindered somewhat by rain contamination and are very sparse in space and time. The impacts of rain are functions of the remotely sensed wavelength and rain–drop size. Therefore, relative long wavelengths have been used to observe the surface, but at the cost of a larger footprint. We examine how smaller footprint sizes could be used to observe through gaps between moderate to heavy rainbands that circulate around the main low-pressure center of a TC. Aircraft data from the National Oceanic and Atmospheric Administration’s (NOAA’s) WP-3D turboprop aircraft will be used to create realistic maps of rain. Our results provide information on the satellite instrument characteristics needed to see the surface through these gaps. This information is expected to aid in developing hurricane-related applications of new higher-resolution satellites.
topic tropical cyclone
rainband gap
satellite
rain rate
threshold
precipitation
url https://www.mdpi.com/2072-4292/12/17/2673
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AT markabourassa analyzinggapsinhurricaneraincoveragetoinformfuturesatelliteproposals
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