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    Seasonal and Synoptic Variations in Near-Surface Air Temperature Lapse Rates in a Mountainous Basin

    Source: Journal of Applied Meteorology and Climatology:;2008:;volume( 047 ):;issue: 001::page 249
    Author:
    Blandford, Troy R.
    ,
    Humes, Karen S.
    ,
    Harshburger, Brian J.
    ,
    Moore, Brandon C.
    ,
    Walden, Von P.
    ,
    Ye, Hengchun
    DOI: 10.1175/2007JAMC1565.1
    Publisher: American Meteorological Society
    Abstract: To accurately estimate near-surface (2 m) air temperatures in a mountainous region for hydrologic prediction models and other investigations of environmental processes, the authors evaluated daily and seasonal variations (with the consideration of different weather types) of surface air temperature lapse rates at a spatial scale of 10 000 km2 in south-central Idaho. Near-surface air temperature data (Tmax, Tmin, and Tavg) from 14 meteorological stations were used to compute daily lapse rates from January 1989 to December 2004 for a medium-elevation study area in south-central Idaho. Daily lapse rates were grouped by month, synoptic weather type, and a combination of both (seasonal?synoptic). Daily air temperature lapse rates show high variability at both daily and seasonal time scales. Daily Tmax lapse rates show a distinct seasonal trend, with steeper lapse rates (greater decrease in temperature with height) occurring in summer and shallower rates (lesser decrease in temperature with height) occurring in winter. Daily Tmin and Tavg lapse rates are more variable and tend to be steepest in spring and shallowest in midsummer. Different synoptic weather types also influence lapse rates, although differences are tenuous. In general, warmer air masses tend to be associated with steeper lapse rates for maximum temperature, and drier air masses have shallower lapse rates for minimum temperature. The largest diurnal range is produced by dry tropical conditions (clear skies, high solar input). Cross-validation results indicate that the commonly used environmental lapse rate [typically assumed to be ?0.65°C (100 m)?1] is solely applicable to maximum temperature and often grossly overestimates Tmin and Tavg lapse rates. Regional lapse rates perform better than the environmental lapse rate for Tmin and Tavg, although for some months rates can be predicted more accurately by using monthly lapse rates. Lapse rates computed for different months, synoptic types, and seasonal?synoptic categories all perform similarly. Therefore, the use of monthly lapse rates is recommended as a practical combination of effective performance and ease of implementation.
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      Seasonal and Synoptic Variations in Near-Surface Air Temperature Lapse Rates in a Mountainous Basin

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    • Journal of Applied Meteorology and Climatology

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    contributor authorBlandford, Troy R.
    contributor authorHumes, Karen S.
    contributor authorHarshburger, Brian J.
    contributor authorMoore, Brandon C.
    contributor authorWalden, Von P.
    contributor authorYe, Hengchun
    date accessioned2017-06-09T16:18:06Z
    date available2017-06-09T16:18:06Z
    date copyright2008/01/01
    date issued2008
    identifier issn1558-8424
    identifier otherams-65317.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206529
    description abstractTo accurately estimate near-surface (2 m) air temperatures in a mountainous region for hydrologic prediction models and other investigations of environmental processes, the authors evaluated daily and seasonal variations (with the consideration of different weather types) of surface air temperature lapse rates at a spatial scale of 10 000 km2 in south-central Idaho. Near-surface air temperature data (Tmax, Tmin, and Tavg) from 14 meteorological stations were used to compute daily lapse rates from January 1989 to December 2004 for a medium-elevation study area in south-central Idaho. Daily lapse rates were grouped by month, synoptic weather type, and a combination of both (seasonal?synoptic). Daily air temperature lapse rates show high variability at both daily and seasonal time scales. Daily Tmax lapse rates show a distinct seasonal trend, with steeper lapse rates (greater decrease in temperature with height) occurring in summer and shallower rates (lesser decrease in temperature with height) occurring in winter. Daily Tmin and Tavg lapse rates are more variable and tend to be steepest in spring and shallowest in midsummer. Different synoptic weather types also influence lapse rates, although differences are tenuous. In general, warmer air masses tend to be associated with steeper lapse rates for maximum temperature, and drier air masses have shallower lapse rates for minimum temperature. The largest diurnal range is produced by dry tropical conditions (clear skies, high solar input). Cross-validation results indicate that the commonly used environmental lapse rate [typically assumed to be ?0.65°C (100 m)?1] is solely applicable to maximum temperature and often grossly overestimates Tmin and Tavg lapse rates. Regional lapse rates perform better than the environmental lapse rate for Tmin and Tavg, although for some months rates can be predicted more accurately by using monthly lapse rates. Lapse rates computed for different months, synoptic types, and seasonal?synoptic categories all perform similarly. Therefore, the use of monthly lapse rates is recommended as a practical combination of effective performance and ease of implementation.
    publisherAmerican Meteorological Society
    titleSeasonal and Synoptic Variations in Near-Surface Air Temperature Lapse Rates in a Mountainous Basin
    typeJournal Paper
    journal volume47
    journal issue1
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/2007JAMC1565.1
    journal fristpage249
    journal lastpage261
    treeJournal of Applied Meteorology and Climatology:;2008:;volume( 047 ):;issue: 001
    contenttypeFulltext
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