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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Spatial and temporal variability of rain-spells characteristics in Serbia and Montenegro
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Spatial and temporal variability of rain-spells characteristics in Serbia and Montenegro

机译:塞尔维亚和黑山的降雨拼写特征的时空变化

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摘要

Rain spells are a key parameter in examining rainfall regime. A rain spell is defined as a series of consecutive days above a certain daily rainfall threshold (DRT). For each rain spell, its duration (RSD), yield (RSY) and average intensity (RSI), as well as their total number (NRS) in each year, were calculated. The present study analyses daily rainfall series from 22 stations representing the different regions of Serbia and Montenegro in the period 1949-2007. This study highlights the temporal variability (both inter- and intra-annual) and the complexity of the rainfall regime in both countries. In each station, all years were divided into three categories: wet, normal and dry according to their standard scores. Then, on the basis of these scores, the entire year was categorized accordingly. The various rain-spell parameters were calculated and are presented for each of these three categories. The relationships between NRS (exponential), RSY (linear) and RSI (power) with the RSD were calculated for each station and their coefficients were plotted. The entire study area was divided into three sub-regions in terms of similar annual behaviour, using the factor analysis. The regions are as follows: northern and central Serbia, eastern and southern Serbia and Montenegro. All years were grouped into several clusters, each representing a different spatial distribution. Their characteristics and probabilities are presented. Overall, Montenegro is much rainier than Serbia, having longer and more intense rain spells. Serbia, on the other hand, has more short rain spells than Montenegro and demonstrates no real summer dryness such as in Montenegro. Intra-annual variability is relatively high in both countries, slightly higher in Montenegro.
机译:降雨过程是检查降雨状况的关键参数。降雨拼写被定义为高于某个每日降雨量阈值(DRT)的一系列连续天。对于每个雨拼,都计算了其持续时间(RSD),产量(RSY)和平均强度(RSI)以及每年的总数(NRS)。本研究分析了代表塞尔维亚和黑山不同地区的22个站点在1949-2007年期间的日降水量序列。这项研究强调了两国的时间变化(年际和年际)以及降雨制度的复杂性。在每个站点中,根据其标准分数,将所有年份分为三类:潮湿,正常和干燥。然后,根据这些分数,对全年进行相应的分类。计算了三种雨拼参数,并针对这三个类别分别进行了介绍。计算每个站的NRS(指数),RSY(线性)和RSI(功率)与RSD之间的关系,并绘制其系数。使用因子分析,按照相似的年度行为将整个研究区域划分为三个子区域。这些地区如下:塞尔维亚北部和中部,塞尔维亚东部和南部以及黑山。所有年份都分为几个集群,每个集群代表不同的空间分布。介绍了它们的特征和概率。总体而言,黑山比塞尔维亚多雨,降雨时间更长且强度更大。另一方面,塞尔维亚的降雨比黑山短,而且没有像黑山那样真正的夏季干旱。两个国家的年内变化都相对较高,黑山的年均变化较高。

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