JáNOSI, IMRE M.World Scientific Publishing CompanyInternational Journal of Bifurcation & ChaosP. Kiss, T. Tel, and I. M. Janosi, 2012: Advection of passive tracers in the atmosphere: Batchelor scaling. Int. J. Bifurcation Chaos, 22, 1250241, doi:10.1142/S0218127412502410....
1.The transfer of a property of the atmosphere, such as heat, cold, or humidity, by the horizontal movement of an air mass:Today's temperatures were higher due to the advection of warm air into the region. 2.The rate of change of an atmospheric property caused by the horizontal movement...
Advection fog formswhen warm, moist air passes over a cool surface. This process is called advection, a scientific name describing the movement of fluid. In the atmosphere, the fluid is wind. When the moist, warm air makes contact with the cooler surface air, water vapor condenses to create...
Coupling of Biennial Oceanic Rossby Waves with the Overlying Atmosphere in the Pacific Basin Anomalies of TOPEX/Poseidon sea level height (SLH), NCEP sea surface temperature (SST), and ECMWF meridional surface wind (MSW) and derived wind stress cur... WB White,Y Chao,C~ Tai - 《J.phys....
At the same time, the cooler water that replaced it at the bottom of the pan has now heated up, become less dense and started to rise. The process starts over again, resulting inconvection currentsthroughout the pan. This same process also occurs in the atmosphere, in the air near a he...
Modeling of these processes is challenging because there is a paucity of sufficiently detailed information on stable temperature inversions in the atmosphere; this is something that UAVs could address. In fallout studies, it is usually assumed that all settling can be explained as the gravitational ...
Although urban air quality and its impacts on the public health have long been studied, the increasing urbanization is raising concerns on how to better control and mitigate these health impacts. A necessary element in predicting exposure levels is fundamental understanding of flow and dispersion in ...
A9220C Chemistry of the oceans A9240F Rivers, runoff, and streamflow A9210M Thermohaline structure and circulation of the oceans A9330N Indian Ocean A9330R Regional seas A9240E Precipitation (hydrological) A9260S Climatology A9260J Water in the atmosphere (humidity, clouds, evaporation, ...
Elucidating the radiative-dynamical coupling between the upper photosphere and deeper atmosphere may be key to our understanding of the abnormally large radii of hot Jupiters. Very long integration times of 3D general circulation models (GCMs) with self-
In the solar atmosphere, the jets are ubiquitous and found to be at various spatia-temporal scales. They are significant to understand energy and mass transport in the solar atmosphere. Recently, the high-speed transition region jets are reported from the observation. Here we conduct a numerical...