考虑到全球气候变化的大高加索、小高加索和塔里什(阿塞拜疆)水文地质块体特征

IF 0.2 Q4 GEOLOGY
I. Tagiyev, V. Kerimov, J. Sherifov
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引用次数: 0

摘要

全球变暖的问题导致了水文和水文地质条件的剧烈变化。里海和山脉对气候的形成有很大的影响。许多人认为气候模型和预测本质上是概率性的,但有些人会认为全球气候变化在今天很重要。有必要考虑到气候变化是全球性的,它发生在我们星球上的任何地方,影响到每个州和每个人。目的:澄清里海的地形和邻近程度的影响,里海决定了气温、降水和其他气候要素的差异和分布。一年的降水量在寒冷的半年以雪的形式出现,雪的融化会引起河流的猛烈的春季洪水,蒸发和充足的相对湿度。气候带的特征与地形的性质和海拔高度的高低密切相关。大高加索、小高加索和塔利什地区的地下水分布在各地。在大高加索地区,主要分布有Kusar组砾石,在Khvalynskaya组、Khazar组、Bakinskaya组和Kusarskaya组内,粘土夹层将一般的地下水流划分为几个层位的压力水,在小高加索地区和Talysh地区也发生了同样的模式。气候变化、降水分布的性质、植物的生长季节、pH-pH值、全球平均气温的上升造成的各种副作用、极端天气事件的频率、水位的上升或下降,最终所有这些都会影响水文河流系统的所有要素和地下水的计算工业储量。森林砍伐是造成全球变暖和温室效应加剧的主要原因之一,对水循环产生负面影响,使蒸腾过程停止。我们应该参与减少二氧化碳排放的过程,关注森林面积的增加,减少水污染,向非常规的可再生太阳能和风能转移,加快引进替代能源矿床的热水。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
CHARACTERISTICS OF HYDROGEOLOGICAL MASSIVES OF THE GREATER, LITTLE CAUCASUS AND TALYSH (AZERBAIJAN) TAKING INTO ACCOUNT GLOBAL CLIMATE CHANGE
Issues of global warming lead to dramatic changes in hydrological and hydrogeological conditions. The Caspian Sea and mountain ranges have a great influence on the formation of the climate. Many believed that climate models and predictions are probabilistic in nature, but some will think that global climate change is important today. It is necessary to take into account that climate change is global, it occurs everywhere on our planet and affects every state and every person. Purpose: Clarification of the influence of the relief and the proximity of the Caspian Sea which determines the differences and distribution of air temperature, precipitation and other climate elements. The annual amount of precipitation falls in the cold half of the year in the form of snow, the melting of which causes violent spring floods on the rivers, evaporation and sufficient relative moisture. The characteristics of climatic zones show their close relationship with the nature of the relief and with the hypsometric position of the terrain above sea level. Ground waters within the Greater, Lesser Caucasus and Talysh are distributed everywhere. In the Greater Caucasus, there are mainly distributed gravels of the Kusar Formation (QIV), and within the Khvalynskaya, Khazar, Bakinskaya and Kusarskaya formations, clay interlayers divide the general flow of groundwater into several horizons of pressure water, the same pattern also takes place in the Lesser Caucasus and Talysh. Climate change, the nature of precipitation distribution, the growing season of plants, pH-pH, an increase in the average global temperature causing various side effects, the frequency of extreme weather events, a rise or decrease in the water level, ultimately all this affects all elements of the hydrological river systems and calculated industrial reserves of groundwater. Deforestation contributes to global warming and one of the main reasons for the intensification of the greenhouse effect, negatively affects the water cycle, the transpiration process stops. We should participate in the process of reducing CO2 emissions, pay attention to the increase of forest areas, reduction of water pollution, transfer to unconventional renewable solar and wind power, accelerate the introduction of alternative energy deposits of thermal waters.
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