Interannual Variability of Winter Rainfall in Upper Myanmar

Kyaw Than Oo
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引用次数: 2

Abstract

Upper Myanmar region, roughly located between 21° 00' N and 28° 30' N latitude and 92° 10' E and 101° 11' E longitude, is the place where the winter cold season contributes ~2% of the annual total rainfall. The rainfall associated with Western disturbances is small in quantum but veritably important for the cold season crops, maintaining the glaciers over the Putao region, hydropower generation for the whole country and hazard of Jade mining of the Upper Myanmar area. This study aims to find interannual variability and related ocean-atmospheric pattern link with Upper Myanmar cold season rainfall by using great-resolution reanalysis data (ERA5) during 1990-2020. Correlation analysis to test the validation of ERA5 gridded data with the observed data from 25 stations across Myanmar, showed a strong correlation value in the same period that enough reliable for best analysis results. An anomalous anticyclonic (cyclonic) circulation persists over the southern part of the Bay of Bengal and South China sea during wet (dry) years. Also, the warming over the Indian Ocean and the cooling over the Tibetan plateau region correspond to south-north transport of moisture, ensuing in positive rainfall anomalies over the study region during winter. The wide patches of strong negative (positive) correlation are found over the Pacific Ocean, the Atlantic Ocean, Mediterranean Sea (MED), Arabian Sea (ARS), and Red Sea (RED) during wet (dry) years. The link implies that NPO, SPO, and MED have an impact on the winter rainfall inter-annual variability. In addition, the cooling (warming) over the Indochina and western Pacific regions influences the Hadley and Walker circulation bringing above (below) normal rainfall, respectively, over Upper Myanmar. The reply of indices (PO, MED, NINO3.4, IOD, and WDs) on winter rainfall, necessary to further investigation. The complete analysis of winter rainfall aids in the understanding of past extreme events as well as the forecasting and monitoring of drought and floods in Upper Myanmar.
上缅甸冬季降水的年际变化
上缅甸地区大致位于北纬21°00′~ 28°30′,东经92°10′~ 101°11′之间,冬季寒冷季节占全年总降雨量的2%左右。与西部扰动相关的降雨量很小,但对于寒冷季节的作物,维持普桃地区的冰川,全国的水力发电以及上缅甸地区玉石开采的危害至关重要。利用1990-2020年的高分辨率再分析资料(ERA5),研究了缅甸上寒季降水的年际变化及其相关海气格局。对ERA5格网数据与缅甸25个站点的观测数据进行了相关性分析,结果表明,ERA5格网数据与缅甸25个站点的观测数据具有较强的同期相关性,分析结果足够可靠。在湿(干)年,孟加拉湾南部和南海上空持续存在异常的反气旋(气旋)环流。此外,印度洋的变暖和青藏高原地区的变冷与水汽的南北输送相对应,导致研究区冬季出现正降水异常。在湿(干)年,在太平洋、大西洋、地中海(MED)、阿拉伯海(ARS)和红海(Red)上发现了广泛的强负(正)相关斑块。这种联系表明NPO、SPO和MED对冬季降水年际变化有影响。PO、MED、NINO3.4、IOD、WDs等指标对冬季降水的响应,需要进一步研究。对冬季降雨的全面分析有助于了解过去的极端事件以及对上缅甸干旱和洪水的预测和监测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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