首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Changes in daily climate extremes in the eastern and central Tibetan Plateau during 1961–2005
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Changes in daily climate extremes in the eastern and central Tibetan Plateau during 1961–2005

机译:1961-2005年青藏高原东部和中部每日极端气候变化

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摘要

Changes in indices of climate extremes are analyzed on the basis of daily maximum and minimum surface air temperature and precipitation at 71 meteorological stations with elevation above 2000 m above sea level in the eastern and central Tibetan Plateau (TP) during 1961–2005. Twelve indices of extreme temperature and nine indices of extreme precipitation are examined. Temperature extremes show patterns consistent with warming during the studied period, with a large proportion of stations showing statistically significant trends for all temperature indices. Stations in the northwestern, southwestern, and southeastern TP have larger trend magnitudes. The regional occurrence of extreme cold days and nights has decreased by ?0.85 and ?2.38 d/decade, respectively. Over the same period, the occurrence of extreme warm days and nights has increased by 1.26 and 2.54 d/decade, respectively. The number of frost days and ice days shows statistically significant decreasing at the rate of ?4.32 and ?2.46 d/decade, respectively. The length of growing season has statistically increased by 4.25 d/decade. The diurnal temperature range exhibits a statistically decreasing trend at a rate of ?0.20°C per decade. The extreme temperature indices also show statistically significant increasing trends, with larger values for the index describing variations in the lowest minimum temperature. In general, warming trends in minimum temperature indices are of greater magnitude than those for maximum temperature. Most precipitation indices exhibit increasing trends in the southern and northern TP and show decreasing trends in the central TP. On average, regional annual total precipitation, heavy precipitation days, maximum 1-day precipitation, average wet days precipitation, and total precipitation on extreme wet days show nonsignificant increases. Decreasing trends are found for maximum 5-day precipitation, consecutive wet days, and consecutive dry days, but only the last is statistically significant.
机译:根据1961-2005年青藏高原东部和中部71个海拔高于2000 m的气象站的每日最高和最低地表气温和降水,分析了极端气候指数的变化。检查了十二个极端温度指数和九个极端降水指数。极端温度显示出与研究期间变暖相一致的模式,大部分台站对所有温度指数均显示出统计学上的显着趋势。西北,西南和东南TP站的趋势幅度较大。极端寒冷的白天和黑夜的区域发生分别减少了约0.85 d /?d和?2.38 d /十年。在同一时期,极端温暖的白天和黑夜的发生分别增加了1.26 d /十年和2.54 d /十年。霜冻天数和冰冻天数显示出统计学上显着的下降趋势,分别为?4.32和?2.46 d /十年。据统计,生长季节的长度每十年增加4.25 d。昼夜温度范围在统计学上呈下降趋势,速率为每十年约0.20°C。极端温度指数还显示出统计学上显着的上升趋势,其中较大的指数值描述了最低最低温度的变化。通常,最低温度指数的变暖趋势要比最高温度的变暖幅度大。大多数降水指数在TP的南部和北部显示出增加的趋势,而在TP的中间显示出下降的趋势。平均而言,区域年总降水量,强降水天数,最大1天降水量,平均湿日降水量和极端湿日总降水量没有显着增加。发现最大5天降水,连续湿日和连续干日的下降趋势,但只有最后一次具有统计学意义。

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