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Volumn 49, Issue 9, 2010, Pages 1906-1912
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The influence of downstream diurnal heating on the descent of flow across the Sierras
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Author keywords
[No Author keywords available]
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Indexed keywords
AIR MASS;
AIRCRAFT FLIGHT;
CALIFORNIA;
FLOWTHROUGH;
POTENTIAL TEMPERATURE;
SIERRA NEVADA;
STRATIFIED FLOWS;
UPSTREAM CONDITIONS;
VALLEY FLOOR;
VERTICAL VELOCITY;
WEATHER STATIONS;
FLOORS;
HEATING;
SOLAR HEATING;
LANDFORMS;
AIR MASS;
AIR TEMPERATURE;
AIRBORNE SURVEY;
AIRFLOW;
BOUNDARY LAYER;
DIURNAL ACTIVITY;
FOEHN;
HEATING;
OBSERVATIONAL METHOD;
STRATIFIED FLOW;
TOPOGRAPHIC EFFECT;
VALLEY;
CALIFORNIA;
OWENS VALLEY;
SIERRA NEVADA [CALIFORNIA];
UNITED STATES;
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EID: 77957748265
PISSN: 15588424
EISSN: None
Source Type: Journal
DOI: 10.1175/2010JAMC2516.1 Document Type: Article |
Times cited : (36)
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References (10)
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