arXivDaily arXiv每日学术速递 周一至周五更新
arXiv周末暂无论文更新,休息一下吧,周末愉快~~
arXiv 2104.12306physics.ao-ph
收藏

关于全印度降雨指数与印度次区域降雨异质性的研究

On the all-India rainfall index and sub-India rainfall heterogeneity

Spencer A Hill, Adam H Sobel, Michela Biasutti, Mark A Cane

AI总结:

本研究利用120年数据重新审视了AIRI、印度次区域降雨、ENSO与IOD的关系,发现移除ENSO线性影响后IOD与AIRI时间序列显著相关。

摘要:

我们使用120年的海表温度和高分辨率降雨数据集,重新审视了关于全印度降雨指数(AIRI)、印度次区域夏季降雨变化、El Niño-Southern Oscillation(ENSO)和Indian Ocean Dipole(IOD)之间关系的长期争议。AIRI与湿润异常的空间范围及网格点降雨日数的平均值密切跟踪。首降雨变化模态是一个单极子,主要与降雨日数和ENSO相关。第二模态是一个三极子,在高降雨的Western Ghats和Central Monsoon Zone区域具有相同符号载荷,而在其间的东南部印度具有相反符号载荷。IOD投影到该三极子上,因此与AIRI弱相关。然而,当移除ENSO的线性影响时,IOD降雨回归变得准均匀地更偏正,使得去除ENSO残差的IOD与AIRI时间序列显著相关。

英文摘要:

We revisit long-standing controversies regarding relationships among the all-India rainfall index (AIRI), sub-India summer rainfall variations, El Niño-Southern Oscillation (ENSO), and the Indian Ocean Dipole (IOD) using 120-year sea surface temperature and high-resolution rainfall datasets. AIRI closely tracks with the spatial extent of wet anomalies and with the average across gridpoints in rainy day count. The leading rainfall variability mode is a monopole associated primarily with rainy day count and ENSO. The second mode is a tripole with same-signed loadings in the high-rainfall Western Ghats and Central Monsoon Zone regions and opposite-signed loadings in Southeastern India between. The IOD projects onto this tripole and, as such, is weakly correlated with AIRI. However, when the linear influence of ENSO is removed, the IOD rainfall regressions become quasi-homogeneously more positive, making the ENSO-residual IOD and AIRI timeseries significantly correlated.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑