丽江市及其周边地区气候特征

A. Milanović
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引用次数: 1

摘要

利吉市境内位于Podrinje-Colubara地区,属温带大陆性气候,属大陆性雨气候。这是一个丘陵山区,海拔848米(Rajac山),相对高度723米,在这里,利吉江及其支流的山谷被深深切割(高达500米)。这些地貌特征决定了该地区的气流方向,因此,黎吉市部分地区为温带大陆性气候(如山谷),部分地区为严重大陆性气候(如拉惹山)。降水高峰出现在春末夏初的5月和6月,最干燥的月份是2月和10月。对黎吉市及其地区气候变化影响较大的是潘尼亚期北部低洼地区,该地区为北、西北和西方向的湿冷气流的渗透打开了通道。这个位于丽鸡市南部的山区是南方冷空气的“大坝”,所以这里的气温相当低。根据塞尔维亚共和国水文气象研究所1961-1990年的气象年刊资料,提出了气候概况。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Climatic features of Ljig municipal and its surrounding area
Territory of Ljig municipal is located in Podrinje-Colubara region and belongs to the temperate continental climate with continental rain regime. This is hilly- mountainous area with 848 m altitude (Rajac Mountain) and 723 m relative height, in which are deeply incised (up to 500 m) valleys of Ljig River and its tributaries. These geomorphologic features cause airstreams direction in this territory, and because of that some parts of Ljig municipal have temperate continental climate (like valleys) and some of them have severe continental climate (like Rajac Mountain). The peak of precipitation is at the end of spring and beginning of summer - in May and June, and the driest months are February and October. The great influences on climatic changes in Ljig municipal and its area have north low parts of Panonian area, which are open for penetration of damp and cold air streams from north, northwest and west. This mountain area on south part of Ljig municipal is some kind of "dam" for cold air streams from south, so they are considerable colder on this territory. On the base of available data in period 1961-1990 from Meteorological Annuals of Republic Hydrometeorological Institute of Serbia climatologic overview is presented.
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