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Titlebook: Dying and Dead Seas Climatic Versus Anthropic Causes; Jacques C. J. Nihoul,Peter O. Zavialov,Philip P. M Conference proceedings 2004 Sprin

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书目名称Dying and Dead Seas Climatic Versus Anthropic Causes
编辑Jacques C. J. Nihoul,Peter O. Zavialov,Philip P. M
视频video
丛书名称NATO Science Series: IV:
图书封面Titlebook: Dying and Dead Seas Climatic Versus Anthropic Causes;  Jacques C. J. Nihoul,Peter O. Zavialov,Philip P. M Conference proceedings 2004 Sprin
描述There are incentive indications that the growth of human population, the increasing use and abuse of natural resources combined with climate changes (probably due to anthropic pollution, to some extent) exert a considerable stress on closed (or semi-enclosed) seas and lakes. In many regions of the world, marine and lacustrine hydrosystems are (or have been) the object of severe or fatal alterations, from changes in regional hydrological regimes and/or modifications of the quantity or the quality of water resources associated with (natural or man-made) land reclamation, deterioration of geochemical balances (increased salinity, oxygen‘s depletion .. . ), mutations of ecosystems (eutrophication, dramatic decrease in biological diversity ... ) to geological disturbances and to the socio-economic perturbations which have been - or may be in the near future - the consequences of them. Seas and lakes are dying all over the world and some may be regarded as already dead and there is an urgent need to try to understand how this is happening and identify the causes of the observed mutations, weighing the relative effects of climatic evolution and anthropic interferences. This book is the ou
出版日期Conference proceedings 2004
关键词Coast; environment; hydrology; remote sensing; satellite; water; hydrogeology
版次1
doihttps://doi.org/10.1007/978-94-007-0967-6
isbn_softcover978-1-4020-1902-9
isbn_ebook978-94-007-0967-6Series ISSN 1568-1238
issn_series 1568-1238
copyrightSpringer Science+Business Media Dordrecht 2004
The information of publication is updating

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Aral Sea Basin Evolution: Geodynamic Aspect,, and surface runoff is virtually zero. Since direct precipitation over the lake comprises only 10% of the water budget, lake-level fluctuations are largely determined by changes in inflow from the Amu Darya and Syr Darya rivers. These rivers originate in the highest part of the Pamir and Tien-Shan
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The Aral Sea Crisis,ation from its surface. Until the 1960s, the Aral was the world’s fourth largest lake in surface area. Over the past four decades, this water body has rapidly and steadily shrunk as countries in the Aral Sea Basin have increasingly taken inflow from its two influents, the Syr Dar’ya and Amu Dar’ya,
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Main Features of the Caspian Sea Hydrology,rtance to human societies of the vast Caspian region. In these circumstances, improving theoretical and applied knowledge of the sea is indispensable for addressing many complex issues. Specifically, there has been increasing environmental concern over expanding extraction of hydrocarbons off and on
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Contamination of the Caspian Sea: An Overview on Recent Findings,esent of approximately 27 m below the level of the world oceans. It lies between 47°13’ and 36°34’ 35“ north latitude and between 46°38’ 39” and 54°44’ 19“ east longitude, surrounded by the five littoral states of Azerbaijan, Russian Federation, Islamic Republic of Iran, Kazakhstan, and Turkmenistan
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