Titlebook: Global Precipitations and Climate Change; Michel Desbois,Fran?oise Désalmand Conference proceedings 1994 Springer-Verlag Berlin Heidelberg

樹木心

Ventricle

Fluctuations of the Indian Monsoon Regime During the Last 170,000 Years: Evidence from Sea Surface Tggest that during stage 5.5 and the early Holocene, the SW monsoon was probably stronger which resulted in higher precipitation and lower surface salinity. In contrast, during the time interval between 90 and 15 kyr and in particular during the glacial stages 6, 2 and substage 5.2 the SW monsoon was

Palatial

不再流行

Global Climate Changes and Humidity Variations Over East Europe and Asia by Historical Dataextremes registered during the time interval (usually several decades) eliminate partly human-induced factors. Application of this technique is exemplified by the records from East European Plain covering the last millennium..A qualitative analysis of climate changes during the last 2,500-3,000 year

anachronistic

Possible Impacts of Climate Change Upon the Water Balance in Central Europen of water balance elements was carried out according to the Zubenok - Budyko complex method. At assessment of climate warming impacts upon changes of relative air humidity and snow cover characteristics was used an empirical correlation method. Two climatological stations (Hurbanovo 115 m a.s.l. an

貪心

Approaches for Regionalization of Precipitation Climates in the Context of Global Climate Change Mon areas of the western tropical Pacific where an ENSO signal in precipitation is shown to be of the same sign, correlation between stations can be relatively low. In the specific example discussed here, the association between Darwin, Australia and the island station of Apia to the east was only r=0.

陰郁

Generator

Natural Variability of the Asian, Indian and African Monsoons over the Last 130 KAnd the desert belts, is presented for the last 130 ka. Long-term arid/humid alternations took place in rough phase with the global cold/warm variations, reflecting a coherent behaviour of the monsoon patterns, cold phases corresponding to an extension of the arid zones to the South, warm phases corr

小歌劇

Oration

Accumulation at the Surface of Polar Ice Sheets: Observation and Modelling for Global Climate Change of the ice flow dynamics, the balance of water between the ocean and the ice sheets, and therefore the global sea level. General Circulation Models (GCMs) of the atmosphere are very popular, and in principle quite appropriate, tools to study the components of a climate change and its consequences,