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书目名称Greenhouse Effect, Sea Level and Drought影响因子(影响力)




书目名称Greenhouse Effect, Sea Level and Drought影响因子(影响力)学科排名




书目名称Greenhouse Effect, Sea Level and Drought网络公开度




书目名称Greenhouse Effect, Sea Level and Drought网络公开度学科排名




书目名称Greenhouse Effect, Sea Level and Drought被引频次




书目名称Greenhouse Effect, Sea Level and Drought被引频次学科排名




书目名称Greenhouse Effect, Sea Level and Drought年度引用




书目名称Greenhouse Effect, Sea Level and Drought年度引用学科排名




书目名称Greenhouse Effect, Sea Level and Drought读者反馈




书目名称Greenhouse Effect, Sea Level and Drought读者反馈学科排名

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Ice Sheets and Sea Level Change as a Response to Climatic Change at the Astronomical Time Scaleiding a time-dependent atmospheric CO. concentration..Extrapolation has been made for the next 100,000 years assuming no human interference at this time scale: the next ice age is expected to occur before 60,000 years AP, the cooling rate between now and then being roughly 0.01 °C per century. The m

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Sea Levelon of the hazards fall into three categories: (a) long-term planning of refuge and evacuation systems, (b) short-term warning systems, and (c) scientific prediction systems..Scientific knowledge of sea level/climate relationships, and of geological factors concerned with crustal uplift or subsidence

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Recent Developments in Research on the Loess in Chinaspan as well as a large spatial distribution. Recent studies in Baoji about 200 km west of Xian in the Weihe River Valley in the southern part of the loess plateau have indicated that it has a time span no less than 2.5 million years..The profile in Baoji shows that there are better developed loess-

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River and Soils Cyclicities Interfering with Sea Level Changesveal the continental evidence of Imbrie’s 100K cycle and Hays’ 400K cycle. It is quite remarkable that the recorded soils in these continental systems all are relict soils of interglacial age. In the coastal fringe area these soil sequences may interfere periodically with interglacial marine deposit

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https://doi.org/10.1007/978-3-030-05165-5mperature to give a composite natura and manmade global temperature which very closely matches measured changes over the past century..The variation of local, regional and global precipitation described by the deterministic model is illustrated over various historical periods with examples from Nort

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Melissa Singletary,Samantha Hagertyep sea record. Our present interglacial, the Holocene, is characterized by fluctuations that include a climatic optimum and periods called “little ice ages”..The paleoclimatic record indicates that changes in temperature do not respond in a gradual way but responds in sharp jumps. A second conclusio