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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Spatiotemporal change in China's frost days and frost-free season, 1955–2000
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Spatiotemporal change in China's frost days and frost-free season, 1955–2000

机译:1955–2000年中国霜冻天数和无霜季节的时空变化

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From 1955 to 2000, China has experienced a decrease in the number of frost days, while the length of the frost-free season between the last spring freeze and the first fall frost has increased. Three distinct regimes can be detected in the time series: up to about 1973, the annual number of frost days was about 2 d higher than the 1961–1990 average; from 1973 to 1985, the annual number of frost days held close to that average with remarkably little interannual variability; and after 1985, the annual number of frost days decreased rapidly with distinct reversal around 1992. The dates of first and last frost show two patterns: before 1980, these dates fluctuated around the 1961–1990 average, but after 1980 (and especially from 1993) the frost-free season was rapidly lengthened. The numbers of frost days are highly correlated with minimum temperature (Tmin) in north China in spring and fall; while in south China frost dates correlate with minimum temperatures in winter. Generally, the seasonal relationships between Tmin and frost days are significant in both the temporal and spatial domains when seasonal average Tmin falls within a range of ±10°C. Analyzing annual and seasonal influences on the number of frost days, we find that water vapor plays a significant role. Regionally, the greater influence on the length of the frost-free season in south China has been the delayed onset of the autumn frost, while in north China the spring and autumn dates each have a comparable influence on the length of the frost-free season. The initial lengthening of the frost-free season lagged about 10 years behind the rapid increase in daily minimum temperatures, while the decrease in the annual number of frost days lagged by about 15 years.
机译:从1955年到2000年,中国的霜冻天数减少了,而从去年春季冰冻到第一次秋季霜冻之间的无霜季节的长度增加了。在时间序列中可以检测到三种不同的状态:直到1973年左右,每年的霜冻天数比1961-1990年的平均值高出约2 d。从1973年到1985年,每年的霜冻天数保持在接近该平均值的水平,并且年际变化很小。 1985年以后,每年的霜冻天数迅速减少,并且在1992年左右发生了明显的逆转。第一次霜冻和最后一次霜冻的日期表现出两种模式:1980年之前,这些日期在1961-1990年平均值附近波动,但是在1980年之后(尤其是从1993年开始) )无霜季节迅速延长。华北地区春季和秋季的霜冻天数与最低温度(Tmin)高度相关。而在华南,霜冻日期与冬季最低温度相关。通常,当季节平均Tmin落在±10°C范围内时,Tmin与霜冻日之间的季节关系在时间和空间域上都很重要。通过分析每年和季节性对霜冻天数的影响,我们发现水蒸气起着重要作用。从地区上看,华南地区无霜季节长度的更大影响是秋季霜冻的推迟出现,而在华北地区,春季和秋季日期对无霜季节的长度都有类似的影响。 。无霜季节的最初延长比每日最低温度的迅速增加落后了约10年,而每年的霜冻天数的减少落后了约15年。

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