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Response Characteristics of Climate in the Shiyang River Basin to Global Warming

机译:石羊河流域气候对全球变暖的响应特征

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摘要

Meteorological data of 5 weather stations in the Shiyang River Basin on the eastern section of Hexi Corridor from 1961 to 2014 were analyzed using statistical analysis techniques such as linear trend and variance signifi cance test. The results showed that as the low temperature rose generally, temperature in stations nearby desert showed higher increase rate; annual extreme maximum temperature in stations nearby mountains showed more signifi cant increase, and annual extreme minimum temperature in stations nearby desert showed more signifi cant increase, and the increase tendency of extreme minimum temperature was more obvious than that of extreme maximum temperature; annual extreme maximum temperature in stations in desert showed higher instability; instability of annual extreme minimum temperature in all sampling points increased, and showed no obvious regularity between desert and mountain.
机译:利用线性趋势和方差显着性检验等统计分析技术,对河西走廊东段石羊河流域1961〜2014年5个气象站的气象资料进行了分析。结果表明,随着低温的普遍升高,沙漠附近站的温度升高速率较高;山区附近气象站的年极端最高气温出现较大幅度的增加,沙漠附近气象站的年极端最低气温出现较大的升高,并且极端最低温度的升高趋势比极端最高温度明显。沙漠站的年度极端最高温度显示出更高的不稳定度;所有采样点的年极端最低温度的不稳定性都增加了,并且沙漠和山脉之间没有明显的规律性。

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