Liste complète des notices publiques
Page 3950/10293
- Sub-seasonal to seasonal prediction. The gap between weather and climate forecasting
- Description de la côte d'Afrique de Ceuta au Sénégal par Valentim Fernandes (1506-1507)
- Lo que hay que leer. 1 Materiales de lectura para estudiantes principiantes de español
- C11004 - Westward movement of eddies into the Gulf of Aden from the Arabian Sea (DOI 10.1029/2006JC004020)
- How to live a low-carbon life: the individual's guide to stopping climate change by Chris Goodall, Earthscan. ix + 319pp. ISBN 978 1 84407 426 6
- C03014 - Hydrogeological modeling of submarine groundwater discharge on the continental shelf of Louisiana (DOI 10.1029/2006JC003557)
- NOWCAST - CHAPTER CHANNEL
- A Porous-Medium Theory for Barotropic Flow through Ridges and Archipelagos
- Atmospheric fate of CF3 OH. 1 : gas phase thermal decomposition
- Modeling soil moisture : a project for intercomparison of land surface parameterization schemes phase 2 [b]
- Biogenic sulfur emissions and aerosols over the tropical south atlantic. 2 . one dimensional simulation of sulfur chemistry in the marine boundary layer
- Az idojaras hatasa az oszi buza mutragyazasanak hatekonysagara
- Extended abstracts of papers presented at the third WMO symposium on meteorological aspects of tropical droughts with emphasis on long-range forecasting [Niamey, Niger, 30 April-4 May 1990]
- Surface-based passive microwave studies of multiyear sea ice
- A SIMPLE MODEL OF NEUTRALLY STRATIFIED BOUNDARY-LAYER FLOW OVER COMPLEX TERRAIN WITH SURFACE ROUGHNESS MODULATIONS [MS3DJH/3R]
- THUNDERSTORMS : WIND SHEAR AND AVIATION SAFETY
- ZUM VERHAELTNIS VON NUMERISCHER ANALYSE UND INITIALISIERUNG
- DETERMINATION SIMPLE DU COEFFICIENT DE DIFFUSIVITE TURBULENTE VERTICALE KZ POUR LA CHALEUR SENSIBLE ET LA QUANTITE DE MOUVEMENT DANS LES PREMIERS METRES AU-DESSUS DU SOL, TENANT COMPTE DE L EFFET RADIATIF
- SEASONAL VARIATION OF INFANT MORTALITY ANALYZED BY CENSUS METHOD
- Evaluation of the importance of Lagrangian canopy turbulence formulations in a soil-plant-atmosphere model
