Titlebook: Clouds, Chemistry and Climate; Paul J. Crutzen,Veerabhadran Ramanathan Conference proceedings 1996 Springer-Verlag Berlin Heidelberg 1996

人造

chapel

,NATO ARW on Clouds — Session Summaries,The two papers presented in this session focused on the role of dynamics in the water vapor distribution of the tropics and its implications to climate.

尾巴

Cleave

牢騷

indubitable

減弱不好

Fazit und weiterer Forschungsbedarf, site above sea level, a.s.l, is 3250 m, Figure 1). One year later, the US Greenland Ice Sheet Project (GISP2) successfully completed a second drilling in the same region at a site located 28 km apart (3208 m a.s.l). These two, more than 3 km long, cores have now been continuously analysed for their

Indelible

Schulsozialarbeit am übergang Schule - Berufst of which are inadequately understood. The spatial scales involved in cloud formation range from tenths of micrometers for cloud condensation nuclei to hundreds of kilometers for large-scale dynamics. Most of these processes cannot be resolved by the current generation of climate models with typic

opalescence

Soziale Arbeit an Sekundarschulen in Berlin,) are within a narrow range between 300 K and 303 K, and less than 0.01% of the ocean surface has SSTs in excess of 304 K (Figure 1). Furthermore, deep convection is triggered only when SSTs exceed 300 K. In regions of deep convection and warm SST, the reduction of outgoing longwave energy by the at

Alpha-Cells