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Intense Tropical Cyclone Emnati was a tropical cyclone that affected Madagascar, only two weeks after Cyclone Batsirai.The sixth tropical disturbance, the second tropical cyclone, and the second intense tropical cyclone of the 2021–22 South-West Indian Ocean cyclone season, Emnati formed from a zone of disturbed weather that was first noted on 15 February 2022.
In geology, a disturbance is a linear zone of disturbed rock strata stretching for many miles across country which comprises a combination of folding and faulting.The British Geological Survey record a number of such features in South Wales including the Neath Disturbance, Pontyclerc Disturbance, Carreg Cennen Disturbance and the Cribarth Disturbance, the latter sometimes also known (at least ...
In meteorology, an invest (short for "investigative area") [1] is a designated area of disturbed weather that is being monitored for potential tropical cyclone development. Invests are designated by three separate United States forecast centers: the National Hurricane Center , the Central Pacific Hurricane Center , and the Joint Typhoon Warning ...
The weather event made damage to many buildings along the coast as well as disrupt railway services due to flooding. [218] On 28 January, Storm Lolita, named by FUB, caused two deaths in Germany. [219] [220] On 14 February, a rapidly deepening low in the Atlantic affected Iceland, named Uta by the Free University of Berlin.
MeteoAlarm.org has been developed for EUMETNET, the European Network of National Meteorological Services who are members of the World Meteorological Organization (WMO). The National Meteorological Service of Austria (GeoSphere Austria) is the responsible member for this project and does the technical realisation.
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AccuWeather's Europe summer forecast highlights the zone from northern France to Germany, Poland and into the Balkan states as the most likely corridor to face more frequent bouts of precipitation ...
Cyclogenesis is the development and strengthening of cyclonic circulations, or low-pressure areas, within the atmosphere. [3] Cyclogenesis is the opposite of cyclolysis, and has an anticyclonic (high-pressure system) equivalent which deals with the formation of high-pressure areas—anticyclogenesis. [4]