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Spatial variations of climate indices in Turkey

机译:土耳其气候指数的空间变化

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The present study explores the spatial variability of the continentality, oceanity and aridity indices in Turkey. Climatic indices are diagnostic tools used to describe climatic conditions and the state of a climate system. In this study, four indices were calculated using the climatic data from 229 meteorological stations in Turkey. The nature of the indices expresses general climatic features such as continentality, marine influences and aridity. The climatic indices used here are the Johansson Continentality (JC) Index, the Kerner Oceanity Index (KOI), the De Martonne Aridity Index (I_(DM)) and the Pinna Combinative (PV) Index. Furthermore, aridity characteristics in Turkey have been examined using the two separate periods (1960-1990 and 1991-2006). To assess the temperature and precipitation patterns in Turkey, the climatic indices were calculated by using monthly temperature and precipitation for the period 1960-2006. According to the results of the KOI, marine climates characteristics were dominant in the Black Sea region than in its Aegean and Mediterranean region. The JC index is used for the climatic classification between continental and oceanic climates. The continental effect was found across 25% of the country. The maximum continentality with a score of 71.5 has been found in the eastern Anatolia. Furthermore, semi-dry areas were increasing in the 1991-2006 period compared to 1960-1990. A significant correlation was found between the values of the JC index and the KOI. The JC index gives reasonable results for Turkey. The continental effect was found across 25% of the country. This analysis may be of benefit for the explanation of landscape characteristics and the rational utilization of water resources, agriculture and energy scenarios for the region in many areas of Turkey.
机译:本研究探讨了土耳其大陆,海洋和干旱指数的空间变异性。气候指数是用于描述气候条件和气候系统状态的诊断工具。在这项研究中,使用来自土耳其229个气象站的气候数据计算了四个指数。指数的性质表示总体气候特征,例如大陆性,海洋影响和干旱。这里使用的气候指数是约翰逊大陆性(JC)指数,克纳海洋性指数(KOI),马田干旱指数(I_(DM))和品纳综合指数(PV)。此外,土耳其的干旱特征已通过两个不同的时期(1960-1990年和1991-2006年)进行了研究。为了评估土耳其的温度和降水模式,使用1960-2006年期间的每月温度和降水量来计算气候指数。根据KOI的结果,黑海地区的海洋气候特征比爱琴海和地中海地区的优势多。 JC指数用于大陆和海洋气候之间的气候分类。在全国25%的地区都发现了大陆效应。在安纳托利亚东部发现了最大的大陆分,得分为71.5。此外,与1960-1990年相比,1991-2006年期间的半干旱地区有所增加。发现JC指数和KOI之间存在显着相关性。 JC指数为土耳其提供了合理的结果。在全国25%的地区都发现了大陆效应。这种分析可能有助于解释土耳其许多地区的景观特征以及该地区水资源,农业和能源情景的合理利用。

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