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 …

May 15, 2024 · 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 …

Jul 25, 2025 · 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 …

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Tropical Upper Tropospheric Trough (TUTT) A mid-oceanic trough situated in the tropics at 200 mb Formation mechanism usually from complicated mid-latitude interactions Once present, they …

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.

…is these features, known as tropical upper tropospheric troughs, or TUTTs, that are responsible for the large number of tropical cyclones in the western Pacific.

Jul 8, 2025 · 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 …

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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 …