LITTLE AMERICA V MICROMETEOROLOGY PROGRAM DATA AND ANALYSIS

At Little America V the temperature range of each of the 9 coldest months is large, as is the annual range. Minima are controlled by advection of cold air from the interior and maxima by advection of warmer air from the Ross Sea area. The winter lacks a distinct temperature minimum, and mid-winter r...

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Main Authors: Lettau, Heinz H., Wollaston, Sarah H., Dalrymple, Paul C.
Other Authors: WISCONSIN UNIV-MADISON
Format: Text
Language:English
Published: 1967
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0650188
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0650188
id ftdtic:AD0650188
record_format openpolar
spelling ftdtic:AD0650188 2023-05-15T13:35:10+02:00 LITTLE AMERICA V MICROMETEOROLOGY PROGRAM DATA AND ANALYSIS Lettau, Heinz H. Wollaston, Sarah H. Dalrymple, Paul C. WISCONSIN UNIV-MADISON 1967-01 text/html http://www.dtic.mil/docs/citations/AD0650188 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0650188 en eng http://www.dtic.mil/docs/citations/AD0650188 Approved for public release; distribution is unlimited. DTIC AND NTIS Meteorology *ANTARCTIC REGIONS *MICROMETEOROLOGY MEASUREMENT TEMPERATURE STABILITY WIND PERMAFROST CURVE FITTING PERIODIC VARIATIONS WEATHER FORECASTING CLIMATE CORRELATION TECHNIQUES Text 1967 ftdtic 2016-02-22T08:04:08Z At Little America V the temperature range of each of the 9 coldest months is large, as is the annual range. Minima are controlled by advection of cold air from the interior and maxima by advection of warmer air from the Ross Sea area. The winter lacks a distinct temperature minimum, and mid-winter reversals of temperature trend occur. Micrometeorological wind and temperature profiles in the lowest 8 m of the atmosphere were recorded at Little America V in 1957, and hourly means of temperature for about 3,000 hours and wind speed for about 500 hours are published as Appendix B of this report. Procedures used to analyze the 1958 micrometeorological data from the South Pole Station are followed in this analysis and results compared with the less complex relationships at the South Pole. Prepared in cooperation with Ohio State Univ., Columbus, Inst. of Polar Studies, Contrib-97. Text Antarc* Antarctic permafrost Ross Sea South pole South pole Defense Technical Information Center: DTIC Technical Reports database Antarctic Little America ENVELOPE(-164.050,-164.050,-78.667,-78.667) Little America V ENVELOPE(-162.367,-162.367,-78.317,-78.317) Ross Sea South Pole
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Meteorology
*ANTARCTIC REGIONS
*MICROMETEOROLOGY
MEASUREMENT
TEMPERATURE
STABILITY
WIND
PERMAFROST
CURVE FITTING
PERIODIC VARIATIONS
WEATHER FORECASTING
CLIMATE
CORRELATION TECHNIQUES
spellingShingle Meteorology
*ANTARCTIC REGIONS
*MICROMETEOROLOGY
MEASUREMENT
TEMPERATURE
STABILITY
WIND
PERMAFROST
CURVE FITTING
PERIODIC VARIATIONS
WEATHER FORECASTING
CLIMATE
CORRELATION TECHNIQUES
Lettau, Heinz H.
Wollaston, Sarah H.
Dalrymple, Paul C.
LITTLE AMERICA V MICROMETEOROLOGY PROGRAM DATA AND ANALYSIS
topic_facet Meteorology
*ANTARCTIC REGIONS
*MICROMETEOROLOGY
MEASUREMENT
TEMPERATURE
STABILITY
WIND
PERMAFROST
CURVE FITTING
PERIODIC VARIATIONS
WEATHER FORECASTING
CLIMATE
CORRELATION TECHNIQUES
description At Little America V the temperature range of each of the 9 coldest months is large, as is the annual range. Minima are controlled by advection of cold air from the interior and maxima by advection of warmer air from the Ross Sea area. The winter lacks a distinct temperature minimum, and mid-winter reversals of temperature trend occur. Micrometeorological wind and temperature profiles in the lowest 8 m of the atmosphere were recorded at Little America V in 1957, and hourly means of temperature for about 3,000 hours and wind speed for about 500 hours are published as Appendix B of this report. Procedures used to analyze the 1958 micrometeorological data from the South Pole Station are followed in this analysis and results compared with the less complex relationships at the South Pole. Prepared in cooperation with Ohio State Univ., Columbus, Inst. of Polar Studies, Contrib-97.
author2 WISCONSIN UNIV-MADISON
format Text
author Lettau, Heinz H.
Wollaston, Sarah H.
Dalrymple, Paul C.
author_facet Lettau, Heinz H.
Wollaston, Sarah H.
Dalrymple, Paul C.
author_sort Lettau, Heinz H.
title LITTLE AMERICA V MICROMETEOROLOGY PROGRAM DATA AND ANALYSIS
title_short LITTLE AMERICA V MICROMETEOROLOGY PROGRAM DATA AND ANALYSIS
title_full LITTLE AMERICA V MICROMETEOROLOGY PROGRAM DATA AND ANALYSIS
title_fullStr LITTLE AMERICA V MICROMETEOROLOGY PROGRAM DATA AND ANALYSIS
title_full_unstemmed LITTLE AMERICA V MICROMETEOROLOGY PROGRAM DATA AND ANALYSIS
title_sort little america v micrometeorology program data and analysis
publishDate 1967
url http://www.dtic.mil/docs/citations/AD0650188
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0650188
long_lat ENVELOPE(-164.050,-164.050,-78.667,-78.667)
ENVELOPE(-162.367,-162.367,-78.317,-78.317)
geographic Antarctic
Little America
Little America V
Ross Sea
South Pole
geographic_facet Antarctic
Little America
Little America V
Ross Sea
South Pole
genre Antarc*
Antarctic
permafrost
Ross Sea
South pole
South pole
genre_facet Antarc*
Antarctic
permafrost
Ross Sea
South pole
South pole
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0650188
op_rights Approved for public release; distribution is unlimited.
_version_ 1766061780447002624