Concept

Rapid intensification

In meteorology, rapid intensification is a situation where a tropical cyclone intensifies dramatically in a short period of time. The United States National Hurricane Center defines rapid intensification as an increase in the maximum sustained winds of a tropical cyclone of at least in a 24-hour period. In order for rapid intensification to occur, several conditions must be in place. Water temperatures must be extremely warm (near or above ), and water of this temperature must be sufficiently deep such that waves do not churn deeper cooler waters up to the surface. Wind shear must be low; when wind shear is high, the convection and circulation in the cyclone will be disrupted. Dry air can also limit the strengthening of tropical cyclones. Usually, an anticyclone in the upper layers of the troposphere above the storm must also be present for extremely low surface pressures to develop. This is because air must be converging towards the low pressure at the surface, which then forces the air to rise very rapidly in the eyewall of the storm. Due to conservation of mass, this requires a divergence of wind at the top of the troposphere. This process is aided by an upper-level anticyclone which helps efficiently channel this air away from the cyclone. Hot towers have been implicated in tropical cyclone rapid intensification, though they have diagnostically seen varied impacts across basins. The United States National Hurricane Center previously defined rapid deepening of a tropical cyclone, when the minimum central pressure decreased by over a 24-hour period. Currently it is defined as an increase in the maximum sustained winds of a tropical cyclone of at least in a 24-hour period. However, recent research suggests that mean sea level pressure is a better predictor of damage from hurricanes making landfall in the continental United States. The later half of the 21st century forecasts envision stronger greenhouse gas forcing dominating natural variability which along with warming sea surface temperatures will create more intense hurricanes along the U.

About this result
This page is automatically generated and may contain information that is not correct, complete, up-to-date, or relevant to your search query. The same applies to every other page on this website. Please make sure to verify the information with EPFL's official sources.

Graph Chatbot

Chat with Graph Search

Ask any question about EPFL courses, lectures, exercises, research, news, etc. or try the example questions below.

DISCLAIMER: The Graph Chatbot is not programmed to provide explicit or categorical answers to your questions. Rather, it transforms your questions into API requests that are distributed across the various IT services officially administered by EPFL. Its purpose is solely to collect and recommend relevant references to content that you can explore to help you answer your questions.