temperature anomaly वाक्य
उदाहरण वाक्य
मोबाइल
- The hydrothermal system it exploits is one of the largest in the western United States, with temperature anomalies of up to per kilometer.
- However the index is labeled " Temperature Anomaly " with a spread of-. 6 to + . 6 C . Which is it?
- This was based on the expected and predicted ENSO conditions, and the existence of the Pacific warm pool of sub-surface temperature anomalies in this region.
- Temperature anomalies found in coastal locations are exceptional, with R�st and V�r�y lacking a meteorological winter in spite of being north of the Arctic Circle.
- The winter temperatures in southern Lofoten represent the highest temperature anomaly in the world relative to latitude due to the Gulf Stream from the Caribbean Sea.
- This was based on the ENSO Neutral conditions, and the existence of the warm pool of sea surface and sub surface temperature anomalies near the dateline.
- "El Ni�o " and " La Ni�a " are opposite surface temperature anomalies of the Southern Pacific, which heavily influence the weather on a large scale.
- Global ( land and ocean ) surface temperature anomaly time series with new analysis ( solid black ) versus no corrections for time-dependent biases ( blue ).
- :: According to satellite data, global average temperature anomalies jumped from + 0.29C in December 2009 to + 0.72C in January 2010 . ~ U ) 00 : 54, 20 February 2010 ( UTC)
- This is in stark contrast to El Ni�o, which can often develop as warm sea surface temperature anomalies that migrate west from the coast of South America or migrate east from the central Pacific.
- The intent of the hypothesis was to explain climate induced temperature anomalies ( as a result of climate change ) on fish stocks and the proper management strategies that could be associated with such changes.
- They also found that the rate of temperature change was larger than at any time in instrument history, and conclude that the recent El Ni�o was not totally responsible for the large temperature anomaly in 1998.
- A major difference between El Ni�o and the Atlantic Ni�o is that the sea surface temperature anomalies are strictly constrained to the equator in the Atlantic case, while greater meridional extent is observed in the Pacific.
- It turns out that the sea surface temperature anomaly is still in force, an average of three to four degrees above normal along the California coast and as much as nine degrees above normal 100 miles offshore.
- However, in the last two decades, nontraditional El Ni�os were observed, in which the usual place of the temperature anomaly ( Ni�o 1 and 2 ) is not affected, but an anomaly arises in the central Pacific ( Ni�o 3.4 ).
- The "'cold blob "'in the North Atlantic describes a cold temperature anomaly of ocean surface waters, affecting the Atlantic Meridional Overturning Circulation ( AMOC ) which is part of the thermohaline circulation, possibly related to Greenland ice melt from global warming.
- The Pacific Decadal Oscillation "'index "'is the leading empirical orthogonal function ( EOF ) of monthly sea surface temperature anomalies ( "'SST "'- A ) over the North Pacific ( poleward of 20?N ) after the global average sea surface temperature has been removed.
- On August 29, 2016 in commemoration of the International Geological Congress voting 30 to 3 in favor of formally designating the Anthropocene, the artist had NASA s GISTEMP ( global temperature anomalies 5-year mean ) index tattooed onto his arm, on the day of the announcement.
- The Atlantic Ni�o is characterized by a sea surface temperature anomaly centered on the equator between 0?and 30�W . Unlike its Pacific counterpart, the Atlantic Ni�o does not have sea surface temperature anomalies that switch sign from east to west, but rather a single basin-wide anomaly.
- The Atlantic Ni�o is characterized by a sea surface temperature anomaly centered on the equator between 0?and 30�W . Unlike its Pacific counterpart, the Atlantic Ni�o does not have sea surface temperature anomalies that switch sign from east to west, but rather a single basin-wide anomaly.
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