What does this research mean for the field?

Increased vertical wind shear causes the upper-level warm-core structure of mature tropical cyclones to descend, resulting in a shallower balanced vortex. Novelty: ClaimNovelty.INCREMENTAL. Consensus alignment: ConsensusAlignment.NEUTRAL.

October 1, 2004Monthly Weather Review

On the Influences of Vertical Wind Shear on Symmetric Tropical Cyclone Structure Derived from AMSU

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Authors

JKJohn A. KnaffNational Oceanic and Atmospheric Administration SSStacey A. Seseske MDMark DeMariaCooperative Institute for Research in Environmental Sciences

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Cite This Study

Knaff et al. (2004) studied this question.

synapsesocial.com/papers/6a0971f316dfdfe7ed341840 https://doi.org/10.1175/1520-0493(2004)132<2503:otiovw>2.0.co;2

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October 1, 2004Monthly Weather Review

On the Influences of Vertical Wind Shear on Symmetric Tropical Cyclone Structure Derived from AMSU

View Full Paper

Ask AI

Bookmark

Authors

JKJohn A. KnaffNational Oceanic and Atmospheric Administration SSStacey A. Seseske MDMark DeMariaCooperative Institute for Research in Environmental Sciences

Discussion

Member takes

Implication

Key Points

Key points are not available for this paper at this time.

Cite This Study

Knaff et al. (2004) studied this question.

synapsesocial.com/papers/6a0971f316dfdfe7ed341840 https://doi.org/10.1175/1520-0493(2004)132<2503:otiovw>2.0.co;2

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