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    Winter Albedo Characteristics at St. Paul, Minnesota

    Source: Journal of Applied Meteorology:;1989:;volume( 028 ):;issue: 003::page 227
    Author:
    Baker, Donald G.
    ,
    Ruschy, David L.
    DOI: 10.1175/1520-0450(1989)028<0227:WACASP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Mean and median daily albedos of the November-April period are presented for a nonforested station in the North Central region of the United States where frozen soil and persistent snow cover are common winter features. Three distinct albedo periods were found, the occurrence of which can be explained by comparison with associated daily records of air temperature and snow depth. These periods are: I) Introduction to Winter, 9?22 November, a transitional period in which snowfalls begin to occur but with insufficient frequency or duration to greatly alter the mean albedo from growing season values; II) the High Albedo Season, 23 November?17 March, that is characterized by mean and median albedos of 50% or higher and by a negatively skewed distribution of albedo values in contrast to periods I and III; and III) the transition period, Introduction to Spring, 18 March?12 April, where late season snowfalls of brief duration occur, but the mean albedo is lower than in period I because of the more common occurrence of moist surfaces due to snowmelt and rains.
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      Winter Albedo Characteristics at St. Paul, Minnesota

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146654
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    contributor authorBaker, Donald G.
    contributor authorRuschy, David L.
    date accessioned2017-06-09T14:02:39Z
    date available2017-06-09T14:02:39Z
    date copyright1989/03/01
    date issued1989
    identifier issn0894-8763
    identifier otherams-11427.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146654
    description abstractMean and median daily albedos of the November-April period are presented for a nonforested station in the North Central region of the United States where frozen soil and persistent snow cover are common winter features. Three distinct albedo periods were found, the occurrence of which can be explained by comparison with associated daily records of air temperature and snow depth. These periods are: I) Introduction to Winter, 9?22 November, a transitional period in which snowfalls begin to occur but with insufficient frequency or duration to greatly alter the mean albedo from growing season values; II) the High Albedo Season, 23 November?17 March, that is characterized by mean and median albedos of 50% or higher and by a negatively skewed distribution of albedo values in contrast to periods I and III; and III) the transition period, Introduction to Spring, 18 March?12 April, where late season snowfalls of brief duration occur, but the mean albedo is lower than in period I because of the more common occurrence of moist surfaces due to snowmelt and rains.
    publisherAmerican Meteorological Society
    titleWinter Albedo Characteristics at St. Paul, Minnesota
    typeJournal Paper
    journal volume28
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1989)028<0227:WACASP>2.0.CO;2
    journal fristpage227
    journal lastpage232
    treeJournal of Applied Meteorology:;1989:;volume( 028 ):;issue: 003
    contenttypeFulltext
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