globalchange  > 气候变化事实与影响
DOI: 10.1175/JCLI-D-12-00161.1
Scopus记录号: 2-s2.0-84874794913
论文题名:
Quantifying the non-gaussianity of wintertime daily maximum and minimum temperatures in the southeast
作者: Stefanova L.; Sura P.; Griffin M.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2013
卷: 26, 期:3
起始页码: 838
结束页码: 850
语种: 英语
Scopus关键词: Alabama ; Anomalies ; Arctic oscillations ; Climate variability ; Extreme events ; Florida ; Georgia ; Maximum and minimum temperatures ; Maximum temperature ; Minimum surfaces ; Minimum temperatures ; National Weather Services ; Network stations ; Nongaussianity ; North Carolina ; Positively skewed ; Southeast United States ; Statistical moments ; Surface temperatures ; Weather stations ; Atmospheric pressure ; Atmospheric temperature ; Climatology ; Higher order statistics ; Statistics ; Weather information services ; Nickel compounds ; Arctic Oscillation ; climate variation ; El Nino-Southern Oscillation ; extreme event ; skewness ; surface temperature ; temperature anomaly ; winter ; Alabama ; Florida [United States] ; Georgia ; North Carolina ; South Carolina ; United States
英文摘要: In this paper the statistics of daily maximum and minimum surface air temperature at weather stations in the southeast United States are examined as a function of the El Niño-Southern Oscillation (ENSO) and Arctic Oscillation (AO) phase. A limited number of studies address how the ENSO and/or AO affect U.S. daily-as opposed to monthly or seasonal-temperature averages. The details of the effect of the ENSO or AO on the higher-order statistics for wintertime daily minimum and maximum temperatures have not been clearly documented. Quality-controlled daily observations collected from 1960 to 2009 from 272 National Weather Service Cooperative Observing Network stations throughout Florida, Georgia, Alabama, and South and North Carolina are used to calculate the first four statistical moments of minimum and maximum daily temperature distributions. It is found that, over the U.S. Southeast, winter minimum temperatures have higher variability than maximum temperatures and La Niña winters have greater variability of both minimum and maximum temperatures. With the exception of the Florida peninsula, minimum temperatures are positively skewed, while maximum temperatures are negatively skewed. Stations in peninsular Florida exhibit negative skewness for both maximum and minimum temperatures. During the relatively warmer winters associated with either a La Niña orAO1, negative skewnesses are exacerbated and positive skewnesses are reduced. To a lesser extent, the converse is true of the El Niño andAO2. The ENSO and AO are also shown to have a statistically significant effect on the change in kurtosis of daily maximum and minimum temperatures throughout the domain. © 2013 American Meteorological Society.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/52028
Appears in Collections:气候变化事实与影响

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作者单位: Center for Ocean-Atmospheric Prediction Studies, The Florida State University, Tallahassee, FL, United States; Center for Ocean-Atmospheric Prediction Studies, Department of Earth, Ocean and Atmosphere Science, The Florida State University, Tallahassee, FL, United States

Recommended Citation:
Stefanova L.,Sura P.,Griffin M.. Quantifying the non-gaussianity of wintertime daily maximum and minimum temperatures in the southeast[J]. Journal of Climate,2013-01-01,26(3)
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