创造性 发表于 2025-3-26 22:07:39
Vegetation History and Climate Changes in Africa North and South of the Equator (10° S to 10° N) Dur are confronted with the fact that areas that have not been influenced by man can rarely be found. The primary question is which vegetation forms allow us to draw conclusions applicable to a nearly natural vegetation. A first step is the estimation of potential quasi-natural vegetation formations un悄悄移动 发表于 2025-3-27 04:24:42
ers, also in those countries that have no access to Cray super computers. Thus, this book will be of interest to all researchers and scientists in the field of climatology. .978-3-642-64089-6978-3-642-59694-0原告 发表于 2025-3-27 06:05:07
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http://reply.papertrans.cn/88/8722/872194/872194_34.png明智的人 发表于 2025-3-27 17:31:58
Book 2000ching are supported with high-end software running on affordable computers, also in those countries that have no access to Cray super computers. Thus, this book will be of interest to all researchers and scientists in the field of climatology. .Assemble 发表于 2025-3-27 18:34:32
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Introductionallow coasts, but worldwide. This includes direct changes because of temperature and precipitation changes, as well as indirect changes such as vegetation belts. In addition, generally overlooked phenomena such as microbiological changes may occur, as C02 is an important factor for several enzyme re窗帘等 发表于 2025-3-28 03:06:06
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One-Dimensional Hydrodynamic Flow in Complex Networks: State of the Art, Some Applications and Generinor importance in the case of small creeks, large rivers adjusting to new equilibria may result in significant changes in erosion, sedimentation, and water discharge. Knowing more about such changes is therefore essential. Fluvial deltas and basins may be simulated by means of one-dimensional mathe肿块 发表于 2025-3-28 11:08:18
Dendroclimatology: A Southern Hemisphere Perspectivedroclimatologists in the Southern Hemisphere need to be aware. (1) Eighty percent of the Southern Hemisphere is covered by water. Heat transport by the Southern Oceans has special relevance as a major determinant of current climates and an influence on how climates were in the past and might be in t