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Tropical upper tropospheric trough - Wikipedia A tropical upper tropospheric trough (TUTT), also known as the mid-oceanic trough, [1] is a trough situated in the upper-level (at about 200 hPa) tropics Its formation is usually caused by the intrusion of energy and wind from the mid-latitudes into the tropics
What is a tropical upper tropospheric trough (TUTT)? - Fox Weather A Tropical Upper Tropospheric Trough (TUTT) is an elongated region of low pressure in the upper atmosphere that can form when there is a significant gradient of sea temperatures or sudden changes in pressures or wind patterns
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TUTT Low - NOAAs National Weather Service - Glossary Tropical Upper-Tropospheric Trough or TUTT Low - A semipermanent trough extending east-northeast to west-southwest from about 35N in the eastern Pacific to about 15 to 20N in the central west Pacific
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A Tropical Upper Tropospheric Trough (TUTT) in Florida Sadler defined the TUTT as an upper trough that lies between upper ridges in the subtropics and ridges in tropical locations The TUTT is a complex system that often enhances convection along its periphery and limits it near its center
09 What is a TUTT? - stason. org 09 What is a "TUTT"? A "TUTT" is a Tropical Upper Tropospheric Trough A TUTT low is a TUTT that has completely cut-off TUTT lows are more commonly known in the Western Hemisphere as an "upper cold low" TUTTs are different than mid- latitude troughs in that they are maintained by subsidence warming near the tropopause which balances
Tropical Upper Tropospheric Trough Forms - Climate Impact Company Discussion: A tropical upper tropospheric trough (TUTT) pattern has developed in the Caribbean Sea The upper trough slowly drifts westward this week and is replaced by a second trough next week a little further to the north