Liste complète des notices publiques
Page 8460/10304
- Rapport d'activité 2022 [Météo-France]
- Linking snow microstructure to its macroscopic elastic stiffness tensor: A numerical homogenization method and its application to 3-D images from X-ray tomography
- The Callendar Effect. By James Rodger Fleming, American Meteorological Society 2007. xvi+155pp. Hardback ISBN 13:978-1-878220-76-9
- Temporal variations of river basin waters from Topex/Poseidon satellite altimetry. Application to the Amazon basin.
- Smoothing the seasonal means of rainfall and runoff in the linear perturbation model (LPM) using the kernel estimator
- Field and wind tunnel investigations of plume dispersion around single surface obstacles
- Influence of subpixel-scale cloud-top structure on reflectances from overcast stratiform clouds layers
- Comparisons of field measurements of carbon dioxide and nitrous oxide fluxes with model simulations for a legume pasture in southeast Australia
- Evapotranspiration and yield of irrigated chickpea
- DESIGN OF RAINGAUGE NETWORK FOR BHARATHAPUZHA AND PERIYAR RIVER BASINS [INDIA] USING GAMMA DISTRIBUTION
- 1987 ECMWF SEMINAR : THE NATURE AND PREDICTION OF EXTRA-TROPICAL WEATHER SYSTEMS. 7-11 SEPTEMBER 1987
- THERMAL COMFORT OF MAN IN DIFFERENT URBAN ENVIRONMENTS
- DYNAMICS OF THE MIDDLE ATMOSPHERE AT SASKATOON [52 DEGREES N, 107 DEGREES W] : A SPECTRAL STUDY DURING 1981, 1982
- ZUR RESONANTEN WECHSELWIRKUNG VON PLANETAREN WELLEN IN EINEM ZWEISCHICHTENMODELL UNTER BERUECKSICHTIGUNG DER EXTERNEN ANREGUNG EINER WELLE - TEIL 1 : DER AMPLITUDENVERLAUF
- OB ISPOL ZOVANII VEROYATNOSTNYKH PROGNOZOV METEOROLOGICHESKIKH USLOVIJ DLYA POSADKI VOZDUSHNYKH SUDOV
- CARATTERISTICHE DELLO STRATO SUPERFICIALE A MILANO LINATE NEL PERIODO ESTIVO
- THE APPLICATION OF NON-LINEAR NORMAL MODE INITIALIZATION TO AN OPERATIONAL FORECAST MODEL
- On the representation of land surface fluxes for atmospheric modelling
- TRANSPORT DER INNEREN UND KINETISCHEN ENERGIE IN DER ATMOSPHARE
- DEUXIEME NOTE SUR LES DISCORDANCES QU'ON OBSERVE ENTRE LES INDICATIONS DE DIVERS THERMOMETRES A L'AIR LIBRE ET A L'OMBRE