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Is Pre-monsoon Rainfall Activity Over India Increasing in the Recent Era of Global Warming?

机译:在最近的全球变暖时代,印度普通季前翁降雨量活动越来越多?

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摘要

The 21 year moving averages of all-India pre-monsoon rainfall (PMR) shows epochal changes. The interesting fact is the presence of an increasing trend during 1970-2015. This change is closely associated with global warming. The tendencies of rainfall during this period are evaluated over India using gridded rainfall data. The differences in the mean rainfall between the global warming period (1970-2015) and the pre-global warming period (1901-1969) are evaluated. It seems that the major area of India is having positive differences and positive tendencies. In this study, the active and weak pre-monsoons are discriminated during 1979-2015. The composite mean differences in the rainfall of active and weak pre-monsoons have been evaluated using the daily gridded rainfall data. And also, the composite mean frequencies and their differences of different rainfall events i.e., wet, dry, very light rain, light rain, moderate rain, rather heavy, heavy rain, very heavy rain and extremely heavy rain days are analyzed. The factors responsible for the spatial and temporal evolution of the rainfall composite patterns are elucidated with the help of changes in the thermal, moisture and circulation patterns over India and neighborhood. The scrutiny reveals that the rainfall of the active/weak pre-monsoons in the recent 37 years is primarily associated with (1) the strengthened/weakened low level circulation, (2) increase/decrease in the convective available potential energy (CAPE), sea surface temperature (SST), vertical integrated moisture flux convergence (VIMFC) and relative humidity (RH) and (3) decrease/increase in the outgoing long-wave radiation (OLR). Furthermore, an attempt is made to understand the concurrent/forecast relationships between PMR and the Atlantic Multi-decadal Oscillation Index (AMO), Effective Strength Index (ESI), Southern Oscillation Index (SOI) and Sunspot number of pre-monsoon/winter season.
机译:全印度的21年迁徙均衡(PMR)显示划船。有趣的事实是在1970 - 2015年期间存在越来越趋势。这种变化与全球变暖密切相关。在此期间降雨趋势在印度使用网格降雨数据进行评估。评估全球变暖期(1970-2015)与全球预热期(1901-1969)之间平均降雨的差异。似乎印度的主要区域具有积极的差异和积极的倾向。在这项研究中,在1979 - 2015年期间,歧视活性和弱的季隆。使用日常网格的降雨数据评估了活性和弱季隆的降雨量的复合平均差异。而且,复合平均频率及其不同降雨事件的差异,即湿,干燥,非常小的雨,小雨,中度雨,相当重,大雨,雨非常大的雨水和极其大雨日都会分析。借助印度和邻域的热敏,水分和循环模式的变化,阐明了负责降雨复合模式的空间和时间演变的因素。审查表明,最近37岁的活跃/弱季隆的降雨主要与(1)加强/弱化低水平循环,(2)增加/减少对流可用潜在能源(CAPE),海表面温度(SST),垂直集成水分助殖助长(VIMFC)和相对湿度(RH)和(3)输出长波辐射(OLR)的降低/增加。此外,尝试了解PMR和大西洋多分型振荡指数(AMO)之间的并发/预测关系(AMO),有效强度指数(ESI),南方振荡指数(SOI)和季旺季的太阳黑子数量。

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