STRATOSPHERIC DESCENT RATES WITHIN THE POLAR VORTEX (U914953)

EPA Identifier: U914953 Title: Stratospheric Descent Rates Within the Polar Vortex Fellow (Principal Investigator): Jeffrey A. Hicke Institution: University of Colorado at Boulder EPA Grant Representative: Dale Manty Project Period: January 1, 1996 - July 15, 1999 Project Amount: $0 RFA: STAR Gradua...

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Published: 2007
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Online Access:http://oaspub.epa.gov/eims/eimsapi.dispdetail?deid=79894
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spelling ftepa:oai:epaEIMS:79894 2023-05-15T14:04:29+02:00 STRATOSPHERIC DESCENT RATES WITHIN THE POLAR VORTEX (U914953) 2007-05-03T05:39:22Z http://oaspub.epa.gov/eims/eimsapi.dispdetail?deid=79894 unknown NATIONAL CENTER FOR ENVIRONMENTAL RESEARCH Text 2007 ftepa 2007-11-21T14:48:18Z EPA Identifier: U914953 Title: Stratospheric Descent Rates Within the Polar Vortex Fellow (Principal Investigator): Jeffrey A. Hicke Institution: University of Colorado at Boulder EPA Grant Representative: Dale Manty Project Period: January 1, 1996 - July 15, 1999 Project Amount: $0 RFA: STAR Graduate Fellowships Research Category: Fellowship - Atmospheric Sciences Description Objective: The objective of this research project is to calculate stratospheric descent rates at various times and locations in the Southern Hemisphere using several temperature, water vapor, and ozone data sets and a radiative transfer model. Approach: The descent rate within the polar vortex using several radiative transfer models and newly acquired data sets has been investigated. The primary radiative transfer model used is the NCAR CCM2 general circulation model radiation code. A more accurate, but computationally expensive, model called MODTRAN also was used for sensitivity tests and comparisons. Three data sets have been used in the cooling rate calculation. The first data set consists of 1994 temperature retrievals from the airborne (High Resolution Interferometer Sounder) instrument in the antarctic polar vortex. These profiles extend from the surface to the aircraft altitude in the lower stratosphere. They are valuable as an independent comparison with data sets used in previous studies of the descent rate. Data from numerical weather prediction model analyses comprise the second data set. The United Kingdom Meteorological Office (UKMO) analyses are primarily used in this study because of the model’s emphasis on the middle atmosphere. The final data set contains balloon soundings at McMurdo Station, Antarctica. Descent rates have been calculated from these data sets, and comparisons to the UKMO analyses have been made. Results of clear sky calculations, as is typical of previous studies, show lower descent rates. Supplemental Keywords: fellowship, polar vortex, stratospheric descent rates, temperature, water vapor, ozone, radiative transfer models, Southern Hemisphere., Ecosystem Protection/Environmental Exposure & Risk, RFA, Scientific Discipline, Atmospheric Sciences, Ecological Effects - Environmental Exposure & Risk, Ecological Indicators, Ecology and Ecosystems, Ecosystem/Assessment/Indicators, Environmental Monitoring, Monitoring/Modeling, atmospheric dispersion models, atmospheric measurements, atmospheric modeling, beach erosion, circulation model, climate, climate model, cyclones, ecological models, extratropical transition, hurricane, tropical cyclones, weather prediction Text Antarc* Antarctic Antarctica Environmental Protection Agency (EPA): Science Inventory Antarctic McMurdo Station ENVELOPE(166.667,166.667,-77.850,-77.850) The Antarctic
institution Open Polar
collection Environmental Protection Agency (EPA): Science Inventory
op_collection_id ftepa
language unknown
description EPA Identifier: U914953 Title: Stratospheric Descent Rates Within the Polar Vortex Fellow (Principal Investigator): Jeffrey A. Hicke Institution: University of Colorado at Boulder EPA Grant Representative: Dale Manty Project Period: January 1, 1996 - July 15, 1999 Project Amount: $0 RFA: STAR Graduate Fellowships Research Category: Fellowship - Atmospheric Sciences Description Objective: The objective of this research project is to calculate stratospheric descent rates at various times and locations in the Southern Hemisphere using several temperature, water vapor, and ozone data sets and a radiative transfer model. Approach: The descent rate within the polar vortex using several radiative transfer models and newly acquired data sets has been investigated. The primary radiative transfer model used is the NCAR CCM2 general circulation model radiation code. A more accurate, but computationally expensive, model called MODTRAN also was used for sensitivity tests and comparisons. Three data sets have been used in the cooling rate calculation. The first data set consists of 1994 temperature retrievals from the airborne (High Resolution Interferometer Sounder) instrument in the antarctic polar vortex. These profiles extend from the surface to the aircraft altitude in the lower stratosphere. They are valuable as an independent comparison with data sets used in previous studies of the descent rate. Data from numerical weather prediction model analyses comprise the second data set. The United Kingdom Meteorological Office (UKMO) analyses are primarily used in this study because of the model’s emphasis on the middle atmosphere. The final data set contains balloon soundings at McMurdo Station, Antarctica. Descent rates have been calculated from these data sets, and comparisons to the UKMO analyses have been made. Results of clear sky calculations, as is typical of previous studies, show lower descent rates. Supplemental Keywords: fellowship, polar vortex, stratospheric descent rates, temperature, water vapor, ozone, radiative transfer models, Southern Hemisphere., Ecosystem Protection/Environmental Exposure & Risk, RFA, Scientific Discipline, Atmospheric Sciences, Ecological Effects - Environmental Exposure & Risk, Ecological Indicators, Ecology and Ecosystems, Ecosystem/Assessment/Indicators, Environmental Monitoring, Monitoring/Modeling, atmospheric dispersion models, atmospheric measurements, atmospheric modeling, beach erosion, circulation model, climate, climate model, cyclones, ecological models, extratropical transition, hurricane, tropical cyclones, weather prediction
format Text
title STRATOSPHERIC DESCENT RATES WITHIN THE POLAR VORTEX (U914953)
spellingShingle STRATOSPHERIC DESCENT RATES WITHIN THE POLAR VORTEX (U914953)
title_short STRATOSPHERIC DESCENT RATES WITHIN THE POLAR VORTEX (U914953)
title_full STRATOSPHERIC DESCENT RATES WITHIN THE POLAR VORTEX (U914953)
title_fullStr STRATOSPHERIC DESCENT RATES WITHIN THE POLAR VORTEX (U914953)
title_full_unstemmed STRATOSPHERIC DESCENT RATES WITHIN THE POLAR VORTEX (U914953)
title_sort stratospheric descent rates within the polar vortex (u914953)
publishDate 2007
url http://oaspub.epa.gov/eims/eimsapi.dispdetail?deid=79894
long_lat ENVELOPE(166.667,166.667,-77.850,-77.850)
geographic Antarctic
McMurdo Station
The Antarctic
geographic_facet Antarctic
McMurdo Station
The Antarctic
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_source NATIONAL CENTER FOR ENVIRONMENTAL RESEARCH
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