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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Changes in precipitation and temperature extremes in Central America and northern South America, 1961–2003
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Changes in precipitation and temperature extremes in Central America and northern South America, 1961–2003

机译:1961–2003年,中美洲和南美洲北部降水和温度极端变化

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摘要

In November 2004, a regional climate change workshop was held in Guatemala with the goal of analyzing how climate extremes had changed in the region. Scientists from Central America and northern South America brought long-term daily temperature and precipitation time series from meteorological stations in their countries to the workshop. After undergoing careful quality control procedures and a homogeneity assessment, the data were used to calculate a suite of climate change indices over the 1961–2003 period. Analysis of these indices reveals a general warming trend in the region. The occurrence of extreme warm maximum and minimum temperatures has increased while extremely cold temperature events have decreased. Precipitation indices, despite the large and expected spatial variability, indicate that although no significant increases in the total amount are found, rainfall events are intensifying and the contribution of wet and very wet days are enlarging. Temperature and precipitation indices were correlated with northern and equatorial Atlantic and Pacific Ocean sea surface temperatures. However, those indices having the largest significant trends (percentage of warm days, precipitation intensity, and contribution from very wet days) have low correlations to El Ni?o–Southern Oscillation. Additionally, precipitation indices show a higher correlation with tropical Atlantic sea surface temperatures.
机译:2004年11月,在危地马拉举行了一次区域气候变化研讨会,其目的是分析极端气候在该地区的变化。来自中美洲和南美洲北部的科学家将其国家气象站的长期日温度和降水时间序列带到了讲习班。经过仔细的质量控制程序和同质性评估之后,这些数据被用于计算一套1961-2003年期间的气候变化指数。对这些指标的分析显示出该地区的总体变暖趋势。极端温暖的最高和最低温度的发生率增加了,而极端寒冷的温度事件的发生率却降低了。尽管存在较大的和预期的空间变异性,但降水指数表明,尽管没有发现总量的显着增加,但降雨事件正在加剧,并且湿天和非常湿天的贡献正在增加。温度和降水指数与北部和赤道大西洋以及太平洋海表温度相关。然而,那些具有最大显着趋势(暖天百分比,降水强度和非常潮湿的天的贡献)的指数与厄尔尼诺-南方涛动的相关性较低。此外,降水指数显示出与热带大西洋海表温度的更高相关性。

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