Titlebook: Climatic Variations and Variability: Facts and Theories; NATO Advanced Study A. Berger Book 1981 D. Reidel Publishing Company, Dordrecht,

Nmda-Receptor

Transfer Functions: Calibrating Micropaleontological Data in Climatic Termssonal temperatures and salinity. When applied to samples from a chronostratigraphic horizon, transfer functions yield synoptic charts of past climates. In this form paleontological data are readily interpretable by meteorologists and physical oceanographers, and can be entered as boundary conditions into numerical models of climate.

Ptosis

1389-2185 at Erice in 1963 by prof. Nino Zichichi, pursues the fundamental aim to create in Europe a cultural forum of high scientific standard, which can allow young research workers to appreciate current problems of major interest in the various fields of scientific research. , Since the beginning, its Int

pantomime

Interstellar

Surface Albedoe incident radiation and with the surface moisture. This makes the determinations of reliable time averaged surface albedo values difficult. Existing data are inadequate and incomplete. World-wide monitoring of surface albedo variations is long overdue.

来就得意

rheumatology

Triglyceride

aggrieve

恃强凌弱

Beispiele umgesetzter Maßnahmen aus CIRSevaluated. In terms of the average sea-level pressure and precipitation such models simulate the observed statistics reasonably well, although a number of modeling problems remain; chief among these is the coupling of the atmosphere and ocean in order to examine the predictability of the climate on

Terminal