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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Precipitation and temperature of the southwest Caspian Sea region during the last 55 years: their trends and teleconnections with large-scale atmospheric phenomena
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Precipitation and temperature of the southwest Caspian Sea region during the last 55 years: their trends and teleconnections with large-scale atmospheric phenomena

机译:过去55年里里海西南部地区的降水和温度:它们的趋势和与大规模大气现象的遥相关

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摘要

Climate data from the southwest coast of the Caspian Sea (CS) were statistically analysed to find connections with large-scale atmospheric variabilities and regional impacts. The study area is characterized by a subtropical humid climate. This enclave of high precipitation is extremely important for Iranian food production and is recognized for its high biodiversity. The data sets were investigated for inconsistencies before carrying out the main investigations, and several problems have been identified. The results show three distinct climatic periods in the temperature time series since 1956: 1956 to 1975 with values near to the overall mean, 1977 to 1995 with values lower by 0.5 degrees C and from 1996 to 2010 with values higher by 0.5 degrees C. These periods can be positively correlated with rapid sea level changes of the CS. Moreover, an agreement exists between the three climatic periods and the North Atlantic Oscillation (NAO) variability. The sea surface temperature of the southern CS is shown to be the driving force of the 2m temperatures in the study area. While temperature changes are in accordance with NAO variability, the precipitation variations show connections with ENSO and less with NAO. The trends of precipitation during the period are diverse but display mostly a weak decrease, while the trends of temperature display a clear increase, larger than that for global mean temperatures, overlaid with inter-decadal variations.
机译:对里海西南海岸的气候数据进行了统计分析,以发现与大规模大气变化和区域影响有关的联系。研究区域的特点是亚热带湿润气候。高降水量的飞地对于伊朗的粮食生产极为重要,并因其高度的生物多样性而得到认可。在进行主要调查之前,已经对数据集进行了调查,以发现不一致之处,并且发现了一些问题。结果显示,自1956年以来温度时间序列中三个不同的气候周期:1956年至1975年,其值接近总体平均值; 1977年至1995年,其值降低了0.5摄氏度; 1996年至2010年,其值升高了0.5摄氏度。期间可能与CS的快速海平面变化呈正相关。此外,在三个气候周期与北大西洋涛动(NAO)变异性之间存在一致。南部CS的海表温度显示为研究区域2m温度的驱动力。虽然温度变化与NAO的变化一致,但降水变化显示与ENSO的联系,而与NAO的联系较少。在此期间,降水趋势是多样的,但主要表现为微弱的下降,而温度的趋势则显示出明显的上升,大于全球平均温度,并伴有年代际变化。

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