DOI: 10.1175/JCLI-D-11-00170.1
Scopus记录号: 2-s2.0-84861392595
论文题名: Reconciling the spatial distribution of the surface temperature trends in the Southeastern United States
作者: Misra V. ; Michael J.-P. ; Boyles R. ; Chassignet E.P. ; Griffin M. ; O'brien J.J.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2012
卷: 25, 期: 10 起始页码: 3610
结束页码: 3618
语种: 英语
Scopus关键词: Alabama
; Biosphere-atmosphere interaction
; Climate variability
; Cooling trends
; Florida
; Georgia
; North Carolina
; Seasonal cycle
; Seasonality
; South Carolina
; Spatial heterogeneity
; Summer season
; Surface temperatures
; Temperature trends
; Trends
; Urban areas
; Atmospheric temperature
; Climatology
; Feedback
; Irrigation
; Surface properties
; Rural areas
; atmosphere-biosphere interaction
; climate feedback
; climate variation
; climatology
; spatial distribution
; surface temperature
; warming
; Alabama
; Florida [United States]
; Georgia
; North Carolina
; South Carolina
; United States
英文摘要: This study attempts to explain the considerable spatial heterogeneity in the observed linear trends of monthly mean maximum and minimum temperatures (T max and T min) from station observations in the southeastern (SE) United States (specifically Florida, Alabama, Georgia, South Carolina, and North Carolina). In a majority of these station sites, the warming trends in T min are stronger in urban areas relative to rural areas. The linear trends of T min in urban areas of the SE United States are approximately 7°F century -1 compared to about 5.5°F century -1 in rural areas. The trends in T max show weaker warming (or stronger cooling) trends with irrigation, while trends in T min show stronger warming trends. This functionality of the temperature trends with land features also shows seasonality, with the boreal summer season showing the most consistent relationship in the trends of both T max and T min. This study reveals that linear trends in T max in the boreal summer season show a cooling trend of about 0.5°F century -1 with irrigation, while the same observing stations on an average display warming trends in T min of about 3.5°F century -1. The seasonality and the physical consistency of these relationships with existing theories may suggest that urbanization and irrigation have a nonnegligible influence on the spatial heterogeneity of the surface temperature trends over the SE United States. The study also delineates the caveats and limitations of the conclusions reached herein due to the potential influence of perceived nonclimatic discontinuities (which incidentally could also have a seasonal cycle) that have not been taken into account. © 2012 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/52403
Appears in Collections: 气候变化事实与影响
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作者单位: Department of Earth, Ocean and Atmospheric Science, Center for Ocean-Atmospheric Prediction Studies, The Florida State University, Tallahassee, FL, United States; Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC, United States; Center for Ocean-Atmospheric Prediction Studies, Florida Climate Center, The Florida State University, Tallahassee, FL, United States; Department of Earth, Ocean and Atmospheric Science, Center for Ocean-Atmospheric Prediction Studies, and Florida Climate Center, The Florida State University, Tallahassee, FL, United States
Recommended Citation:
Misra V.,Michael J.-P.,Boyles R.,et al. Reconciling the spatial distribution of the surface temperature trends in the Southeastern United States[J]. Journal of Climate,2012-01-01,25(10)