Changes in frost days in simulations of twentyfirst century climate

被引:102
|
作者
Meehl, GA [1 ]
Tebaldi, C [1 ]
Nychka, D [1 ]
机构
[1] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
关键词
D O I
10.1007/s00382-004-0442-9
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Global coupled climate model simulations of twentieth and twentyfirst century climate are analyzed for changes in frost days (defined as nighttime minima less than freezing). The model simulations agree with the observed pattern for late twentieth century of a greater decrease of frost days in the west and southwest USA compared to the rest of the country, and almost no change in frost days in fall compared to relatively larger decreases in spring. Associated with general increases of nighttime minimum temperatures, in the future climate with increased greenhouse gases (GHGs) the number of frost days is fewer almost everywhere, but there are greatest decreases over the western parts of the continents. The numbers of frost days are most consistently related to sea level pressure, with more frost days occurring when high pressure dominates on the monthly time scale in association with clearer skies and lower nighttime minimum temperatures. Spatial patterns of relative changes of frost days are indicative of regional scale atmospheric circulation changes that affect nighttime minimum temperatures. Increases of soil moisture and clouds also contribute, but play secondary roles. The linkages among soil moisture, clouds, sea level pressure, and diurnal temperature range are quantified by a statistical multiple regression model. Coefficients for present and future climate are similar among the predictors, indicating physical processes that affect frost days in present and future climates do not appreciably change. Only the intercept changes in association with the significant warming of the mean climate state. This study highlights the fact that, though there is a general decrease in the number of frost days with global warming, the processes that affect the pattern of those changes, and thus the regional changes of frost days, are influenced by several interrelated physical processes, with changes in regional atmospheric circulation generally being most important.
引用
收藏
页码:495 / 511
页数:17
相关论文
共 50 条
  • [1] Changes in frost days in simulations of twentyfirst century climate
    G. A. Meehl
    C. Tebaldi
    D. Nychka
    Climate Dynamics, 2004, 23 : 495 - 511
  • [2] Recent changes in frost days and the frost-free season in the United States
    Easterling, DR
    BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 2002, 83 (09) : 1327 - 1332
  • [3] Locating Taiwan Cinema in the TwentyFirst Century
    Chun, Tarryn Li-Min
    INTERNATIONAL JOURNAL OF TAIWAN STUDIES, 2024, 7 (01) : 215 - 218
  • [4] Military Ministry: Chaplains in the TwentyFirst Century
    Kocjancic, Klemen
    BOGOSLOVNI VESTNIK-THEOLOGICAL QUARTERLY-EPHEMERIDES THEOLOGICAE, 2023, 83 (02): : 499 - 502
  • [5] Epigenetics comes of age in the twentyfirst century
    Holliday, R
    JOURNAL OF GENETICS, 2002, 81 (01) : 1 - 4
  • [6] The Baer splitting problem in the twentyfirst century
    Griffith, P
    ILLINOIS JOURNAL OF MATHEMATICS, 2003, 47 (1-2) : 237 - 250
  • [7] Epigenetics comes of age in the twentyfirst century
    Robin Holliday
    Journal of Genetics, 2002, 81 : 1 - 4
  • [8] Coupled Model Simulations of Climate Changes in the 20th Century and Beyond
    俞永强
    智海
    王斌
    万慧
    李超
    刘海龙
    李薇
    郑伟鹏
    周天军
    AdvancesinAtmosphericSciences, 2008, (04) : 641 - 654
  • [9] Coupled model simulations of climate changes in the 20th century and beyond
    Yongqiang Yu
    Hai Zhi
    Bin Wang
    Hui Wan
    Chao Li
    Hailong Liu
    Wei Li
    Weipeng Zheng
    Tianjun Zhou
    Advances in Atmospheric Sciences, 2008, 25 : 641 - 654
  • [10] Coupled model simulations of climate changes in the 20th century and beyond
    Yu Yongqiang
    Zhi Hai
    Wang Bin
    Wan Hui
    Li Chao
    Mu Hailong
    Li Wei
    Zheng Weipeng
    Zhou Tianjun
    ADVANCES IN ATMOSPHERIC SCIENCES, 2008, 25 (04) : 641 - 654