نتایج جستجو برای: wind surface temperature

تعداد نتایج: 1091999  

2012
SHAYNE MCGREGOR AXEL TIMMERMANN NIKLAS SCHNEIDER MALTE F. STUECKER MATTHEW H. ENGLAND

During large El Niño events the westerly wind response to the eastern equatorial Pacific sea surface temperature anomalies (SSTAs) shifts southward during boreal winter and early spring, reaching latitudes of 58–78S. The resulting meridional asymmetry, along with a related seasonal weakening of wind anomalies on the equator are key elements in the termination of strong El Niño events. Using an ...

2008
W. TIMOTHY LIU XIAOSU XIE

Using a combination of Quick Scatterometer (QuikSCAT), Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E), and Lagrangian drifter measurements, we demonstrate that wind data alone are not sufficient to derive ocean surface stress (momentum flux) over mid-latitude ocean fronts, specifically the Kuroshio Extension. There was no continuous and large-scale stress measurement ove...

2014
Yang Liu Hui Hu

The in-flight ice formation and accretion are highly dependent on weather conditions that essentially affect the heat transfer capability. When the temperature is sufficiently cold, the heat transfer is adequate to remove all of the latent heat from the collected water. The rate of rime ice accretion is controlled by the droplet collection efficiency. Otherwise, when the heat transfer is inadeq...

Journal: :فیزیک زمین و فضا 0
فرهنگ احمدی گیوی سمانه ثابت قدم عباسعلی علی اکبری بیدختی

mixed layer is a part of the atmospheric boundary layer in which pollutants are uniformly distributed. it is sensitive to the earth’s surface, controls the flow of heat and momentum between the surface and the free atmosphere, thus playing a key role in atmospheric circulation. most of atmospheric pollution models require the height of the mixed layer as an input to determine the depth of atmos...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2004
David W Keith Joseph F Decarolis David C Denkenberger Donald H Lenschow Sergey L Malyshev Stephen Pacala Philip J Rasch

Large-scale use of wind power can alter local and global climate by extracting kinetic energy and altering turbulent transport in the atmospheric boundary layer. We report climate-model simulations that address the possible climatic impacts of wind power at regional to global scales by using two general circulation models and several parameterizations of the interaction of wind turbines with th...

2011
G. J. Steeneveld A. A. M. Holtslag R. T. McNider

[1] Long‐term surface observations over land have shown temperature increases during the last century, especially during nighttime. Observations analyzed by Parker (2004) show similar long‐term trends for calm and windy conditions at night, and on basis of this it was suggested that the possible effect of urban heat effects on long‐term temperature trends are small. On the other hand, a simplif...

2008
X. J. Zheng

In the evolution processes of wind blown sand movement and aeolian geomorphology, it always contains some complex behaviors, for example, the nonlinear character of turbulence and attractors, the stochastic character of wind gust, liftoff and movement of sand, the interaction among wind field, sand movement, electric field in wind blown sand flux and thermal diffusion, multi-scale character fro...

2001
R. A. Pielke T. N. Chase T. G. F. Kittel J. A. Knaff J. Eastman

The value of the analyses of the 200 mbar zonal winds is proposed as a particularly effective tool to assess variability and trends in atmospheric circulation. Using the thermal wind relation, the 200 mbar zonal wind results from the vertically integrated north-south temperature gradient between the Earth’s surface and 200 mbar. We found a tendency for the 200 mbar winds to become somewhat stro...

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