1. A warming ocean and atmosphere along with melting and rising sea levels provide evidence of a dramatic change in the global climate. (P26) 2. Experts claimed that low sea-ice levels caused by climate change meant the bear coul...
A three-dimensional coupled atmosphere-ocean model is developed to study the air-sea interaction processes off the east coast of North America during a winter storm passing over the northwestern Atlantic. The atmospheric component uses the Advanced Regional Prediction System (ARPS) developed at the Ce...
RECENT DEVELOPMENTS OF THE UCLA COUPLED ATMOSPHERE-OCEAN GCM Jin-Yi Yu, Carlos R. Mechoso, John D. Farrara, Young-Joon Kim Jui-Lin Li, Martin Kohler, and Aldo Arakawa Department of Atmospheric Sciences University of California Los Angeles Los Angeles, CA 90095-1565 1. Introduction A fundament...
You might find these chapters and articles relevant to this topic. Atmosphere—Ocean Dynamics In International Geophysics, 1982 9.13 Buoyancy Forcing The ocean–atmosphere system is driven by radiation from the sun (see chapter 1), which produces internal sources of heat within the ocean–atmosphere...
et al. Expanding Tara Oceans protocols for underway, ecosystemic sampling of the ocean-atmosphere interface during Tara Pacific expedition (2016–2018). Front. Mar. Sci. 6, 750 (2019). Article Google Scholar Planes, S. et al. The Tara Pacific expedition — a pan-ecosystemic approach of ...
reanalysis of 1973-1995, we examined interannual atmosphere-ocean variations in the tropical western North Pacific related to the Asian summer monsoon-ENSO ... R Kawamura,T Matsuura,S Iizuka - 《Journal of the Meteorological Society of Japan.ser.ii》 被引量: 48发表: 2002年 Implication of the...
2a)33. In any coupled model experiment, initialised from observational estimates, process representation deficiencies in the atmosphere and ocean model components cause errors in this heat budget. This results in evolving biases in the simulated mixed layer temperature, T, surface heat flux, F, and...
Interactions among the Pacific, Atlantic and Indian Oceans through ocean–atmosphere coupling can initiate and/or modulate climate variability. The Pa
Experiments with an oceanic general circulation model (OGCM) show that both the remotely forced downwelling Kelvin waves and coastal wind anomalies contribute to the extreme coastal El Niño. Atmospheric general circulation model (AGCM) experiments reveal a previously unknown ocean–atmosphere coupling ...
Tides, through the feedback of tidal currents, create a conduit of energy from the ocean to the atmosphere. Part of the tidal energy in the ocean is therefore not dissipated by the bottom drag or internal tides, but by the top drag. To the best of our knowledge, this process is ...