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Climate Changes and Their Teleconnections With ENSO Over the Last 55 Years, 1961–2015, in Floods‐Dominated Basin, Jiangxi Province, China

机译:1961 - 2015年,在中国江西省洪水主导的盆地,气候变化及其与ENSO的联系。

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The relative effect of climate change and El Ni?o–Southern Oscillation (ENSO) is essential not only for understanding the hydrological mechanism over Jiangxi province in China but also for local water resources management as well as flood control. This study quantitatively researched in‐depth information on climate change in Jiangxi using the up‐to‐date “ground truth” precipitation and temperature data, the Asian Precipitation Highly Resolved Observational Data Integration Towards Evaluation of Water Resources (APHRODITE, 1961–2015, 0.25°) data; analyzed the connections between ENSO and climate factors (including precipitation and temperature); and discussed the relationships between the ENSO and climate change. The main findings of this study were (1) during the period of 1961–2015, annual precipitation and temperature generally increased at a rate of 2.68 mm/year and 0.16 °C/10a, respectively; (2) the precipitation temporal trends have significant spatial differences. For example, the high precipitation increasing rates occurred in northern Jiangxi province in summer, while the large decreasing rates happened in most regions of Jiangxi province in spring; (3) an abrupt temperature change was detected around 1984, with general decreasing trends and increasing trends in 1961–1984 and 1984–2015, respectively; (4) ENSO had significant impacts on precipitation changes over Jiangxi province, for example; the El Ni?o events, beginning in April and May, were likely to enlarge the amounts of precipitation in the following summer, and the El Ni?o events beginning in October were likely to enlarge the precipitation amounts in the following spring and summer; and (5) the El Ni?o events, starting in the second half of the year, were likely to raise the temperature in the winter and the following spring. These findings would provide valuable information for better understanding the climate change issues over Jiangxi province.
机译:气候变化和El Ni的相对效果和南方振荡(ENSO)对于了解中国江西省的水文机制,而且对当地水资源管理以及防洪等至关重要。本研究定量地研究了江西气候变化的深入了解,使用最新的“实际”降水和温度数据,亚洲降水高度解决的观测数据集成,以评估水资源(Aphrodite,1961-2015,0.25 °)数据;分析了ENSO和气候因子之间的连接(包括降水和温度);并讨论了恩索与气候变化之间的关系。本研究的主要结果是(1)在1961 - 2015年期间,年降水量和温度通常以2.68毫米/年/年和0.16°C / 10A的速度增加; (2)降水时间趋势具有显着的空间差异。例如,夏季北江北部的高降水率较高,而春季大多数地区发生的大部分地区发生了较大的降低; (3)1984年左右检测地检测到突然的温度变化,分别在1961年至1984年和1984 - 2015年的一般趋势和增加趋势。 (4)ENSO对江西省的降水变化产生了重大影响; El Ni?o活动,从4月和5月开始,可能会在下列夏天扩大降水量,并且埃尔尼·欧盟(El Ni)在10月份开始的活动可能会在以下春夏的降水量扩大; (5)El Ni?O事件,从今年下半年开始,很可能在冬季和以下春天提高温度。这些调查结果将提供有价值的信息,以便更好地理解江西省的气候变化问题。

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