R. D. CESS, • G. L. POTTER, 2 J.P. BLANCHET, 3 G. J. BOER, 3 A.D. DEL GENIO, 4 M. Dl•QUl•, 5 V. DYMNIKOV, 6 V. GALIN, 6 W. L. GATES, 2 S. J. GHAN, 2 J. T. KIEHL, 7 A. A. LACiS, 4 H. LE TREUT, 8 Z.-X. LI, 8 X.-Z. LIANG, 9 B. J. MCAVANEY, lø V. P. MELESHKO, TM J. F. B. MITCHELL, 12 J.-J. MORCRETTE, •3 D. A. RANDALL, TM L. RIKUS, •ø E. ROECKNER, •5 J. F. ROYER, 5 U. SCHLESE, 15 D. A. SHEININ, TM A...

D. A. RANDALL, l R. D. CESS, 2 J.P. BLANCHET, 3 G. J. BOER, 3 D. A. DAZLICH, • A.D. DEL GENIO, 4 M. DEQUE, 5 V. DYMNIKOV, 6 V. GALIN, 6 S. J. GHAN, 7 A. A. LACIS, 4 H. LE TREUT, 8 Z.-X. LI, 8 X.-Z. LIANG, 9 B. J. MCAVANEY, •ø V. P. MELESHKO, TM J. F. B. MITCHELL, •2 J.-J. MORCRETTE, •3 G. L. POTTER, 7 L. RIKUS, lø E. ROECKNER, TM J. F. ROYER, 5 U. SCHLESE, TM D. m. SHEININ, TM J. SLINGO, 15 A. ...

Dynamical seasonal forecasts of tropical storm frequency require robust and efficient algorithms for detection and tracking of tropical storms in atmospheric general circulation models (AGCMs). Tropical storms are generally detected when dynamic and thermodynamic variables meet specified criteria. Here, it is shown that objectively defined modeland basin-dependent detection criteria improve sim...

The Atmospheric Radiation Measurement (ARM) Program, supported by the U.S. Department of Energy, is a major new program of atmospheric measurement and modeling. The program is intended to improve the understanding of processes that affect atmospheric radiation and the description of these processes in climate models. An accurate description of atmospheric radiation and its interaction with clou...

Short-range ocean forecast and reanalysis systems routinely combine observations from satellite altimetry, satellite sea surface temperature (SST), and in situ temperature and salinity, to initialise global and regional ocean models. The most critical observation type for eddy-resolving applications is arguably satellite altimetry. To quantify the impact of satellite altimetry observations on a...

abstract due to low spatial resolution or simplifying of some micrometeorological phenomena, atmospheric general circulation models are not able to give a good estimation for weather conditions over study area. so their outputs should downscale into weather stations scales. in this research data of hadcm3 downscaled by using lars-wg5 with three scenarios, confirmed by ipcc including a1b, a2 and...