WebApr 10, 2024 · In the observation, the El Niño–induced anomalous anticyclonic circulations in the southeast IO trigger downwelling oceanic Rossby waves propagating westward in D(0)JF(1). The Rossby waves reach the tropical Southwest IO (SWIO; 10°S–5°S, 50°E–80°E) after one season where the shallow background thermocline dome locates. http://sxie.ucsd.edu/sio_jc.pdf
Structure and Mechanisms of South Indian Ocean Climate …
WebMar 23, 2024 · The wind stress curl anomalies in the central and eastern of SPNA trigger the topographic and planetary Rossby waves, propagating the downwelling signals along their waveguides to redistribute heat in the upper ocean and warm the Labrador Sea and Irminger Sea with a 4- or 7-year time lag. According to the National Weather Service, atmospheric Rossby waves form primarily as a result of the Earth's geography. Rossby waves help transfer heat from the tropics toward the poles and cold air toward the tropics in an attempt to return atmosphere to balance. They also help locate the jet stream and … See more Waves in the ocean come in many different shapes and sizes. Slow-moving oceanic Rossby waves are are fundamentally different from ocean surface waves. Unlike waves … See more Rossby wave movement is complex. The horizontal wave speed of a Rossby (the amount of time it takes the wave to travel across an ocean basin) is dependent upon the latitude of the … See more office of the mayor of new york
Kelvin Wave - an overview ScienceDirect Topics
WebApr 29, 2013 · The anomalous SSH associated with strong eastward jets propagated eastward as an equatorial Kelvin wave and generated intense downwelling near the eastern boundary. The anomalous positive SSH then partly propagated westward around 4°S as a reflected equatorial Rossby wave, and it significantly influenced the upper … WebDec 1, 2004 · Thus, the downwelling Rossby waves and reflected-equatorial Kelvin waves sustained the warming of the western TIO and west-east temperature gradient from 2024 … office of the mayor of lafayette