沿海降雨模式的长期微尺度年代际分析:南印度小气候变化的指示

IF 0.7 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES
G. Pereira, Gurugnanam Balasubramanian, C. Sabarathinam, S. Goswami, Bairavi Swaminathan
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引用次数: 0

摘要

在全球范围内,降雨和温度的强度和模式存在着巨大的变化。这些变化反映了小气候特征的变化。目前的研究旨在利用沿海地区的月降雨量和平均温度来评估Ramanathapuram沿海地区的气候变化。对三十年(即1990年至2019年)的微尺度降雨和温度趋势进行了分析。研究分为三个不同时期:第一个十年(1990-1999年),第二个十年(2000-2009年)和第三个十年(2010-2020年)。该研究推断,该地区467平方公里的地区在10年内平均降雨量为676毫米。十年来,39平方公里的降雨量为637.6毫米,48平方公里的降雨量为821毫米,只有29平方公里的降雨量为992毫米,但351平方公里的降雨量超过1000毫米。在第三十年,202平方公里的降雨量少于750毫米,43平方公里的降雨量为“亏缺”,24平方公里的降雨量为“过剩”。观测了最近一段时间降雨量的变化。同样,第一个十年(1990-1999)期间气温相对升高。降雨事件的强度、降雨日数和降雨频率反映了变化。陆地表面温度也显示出较小的变化和增加的季间期。降雨量的变化、季风期的变化和气温的变化反映了该地区的小气候变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Long Term Microscale Decadal Analysis of Coastal Rainfall Pattern: An Indication of Microclimatic Variation in South India
There are drastic variations in the intensity and the pattern of rainfall and temperature globally. The variations thus reflect the variation in the microclimatic signatures. The current study aims to assess the climatic changes in the coastal region of Ramanathapuram using the monthly rainfall and temperature average along the coastal region. The microscale rainfall and temperature trend have been analysed for three decades (30 years), representing 1990 to 2019. The study was divided into three different periods: first (1990-1999), second (2000-2009), and the third decade (2010-2020). The study infers that 467 km2 of the area receives an average of 676 mm of rain in decade-I. In decade-II, 39 km2 of the area is noted with 637.6 mm rainfall, 48 km2 of the study area is reported to have 821 mm rainfall, and only 29 km2 area receives normal rainfall of 992 mm, but 351 km2 receives “excess” rainfall of above 1000 mm. In decade-III, less than 750 mm rainfall is recorded at 202 km2, with 43 km2 recorded “deficit” rainfall, and 24 km2 area received an “excess” rainfall. The variation in the amount of rain during the recent period was observed. Similarly, the temperature was comparatively elevated during the Ist Decade (1990-1999). The intensity of rain events, number of rainy days and frequency of rainfall reflected variations. The land surface temperatures also indicated minor variations and increased inter-monsoonal periods. The variation in the rainfall amount, the shift in monsoonal periods and the change in temperature indicate the microclimatic variation in the region.
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来源期刊
Journal of Climate Change
Journal of Climate Change METEOROLOGY & ATMOSPHERIC SCIENCES-
自引率
16.70%
发文量
18
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