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 …

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 …

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 …

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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, …

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 …

…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 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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