Liste complète des notices publiques
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- Heat and health [special section]
- MECI - enregistreurs Speedomax H à porte avec filet d'encadrement, [à] système d'inscription alimenté par tube capillaire, [à] amplificateur transistorisé 444 509, [à] carte d'échelle 1.05 V (licence Leeds & Northrup Company ) : complément à la notice NFE 102 U3 : NFE 102 U3-2 (5-75)
- Evaluation of a Fast-Running Urban Dispersion Modeling System Using Joint Urban 2003 Field Data
- An earth-system perspective of the global nitrogen cycle.
- Use of stabile isotopes and tracers to detect preferential flow patterns in a peatland treating municipal wastewater
- A Combined Local and Nonlocal Closure Model for the Atmospheric Boundary Layer. Part I: Model Description and Testing
- Composition and Chemistry - D24305 - Global modeling of biogenic bromocarbons (DOI 10.1029/2006JD007264)
- Composition and Chemistry - D20304 - Radiative transfer calculations for a passive microwave satellite sensor: Comparing a fast model and a line-by-line model (DOI 10.1029/2005JD006552)
- Catastrophic Flood on the Danube River in August 2002
- An Improved Mellor-Yamada Level-3 Model with Condensation Physics: Its Design and Verification
- Climate and Dynamics (ACL) - ACL 6. High-latitude mesospheric mean winds: A comparison between Tromso (69oN) and Svalbard (78oN) (DOI 10.1029/2003JD003509)
- An observational study of the "interstate 5" dust storm case
- Introduction to wspo Niami's lighthning project throug the examination of a severe weather event
- Structure and reflectance of winter maritime stratocumulus clouds
- Penetration of multiple thundercloud electric fields into the ionosphere
- Modeling the thermal structure of the active layer of the north Atlantic
- STAUBFALL AUF SEE
- GENERATION OF INTERNAL- AND EXTERNAL- MODE MOTIONS FROM INTERNAL HEATING : EFFECTS OF VERTICAL SHEAR AND DAMPING
- O VOZMOZHNOSTI ISPOL ZOVANIYA DANNYKH SETI RAKETNOGO METEOROLOGICHESKOGO ZONDIROVANIYA V DOLGOSROCHNYKH PROGNOZAKH
- Climate variability and trends in SSU radiances : a comparison of model predictions and satellite observation in the middle stratosphere