2008 APS March Meeting
Volume 53, Number 2
Monday–Friday, March 10–14, 2008;
New Orleans, Louisiana
Session H6: Understanding Hurricanes and Severe Storms: Patterns, Prediction and Mitigation
8:00 AM–10:24 AM,
Tuesday, March 11, 2008
Morial Convention Center
Room: RO4
Sponsoring
Unit:
FPS
Chair: Andrew Post-Zwicker, Princeton Plasma Physics Laboratory
Abstract ID: BAPS.2008.MAR.H6.1
Abstract: H6.00001 : Understanding Severe Hurricanes
8:00 AM–8:36 AM
Preview Abstract
Abstract
Author:
Greg J. Holland
(National Center for Atmospheric Research)
Hurricanes are complex phenomena, whose understanding involves
many facets, of which my presentation will provide an overall
flavor and review.
Understanding the physical hurricane involves a complex amalgam
of fluid dynamics, thermodynamics and scale interactions. The
basic structure is one of a fluid vortex, which dictates
everything from the characteristic spiral shape to the clear eye
region. Energetically, once formed a hurricane is a self
sustaining heat engine, one that extracts energy from the
enthalpy difference between the warm ocean surface and the cold
upper atmosphere, and one that will continue its merry way until
it is destroyed by some external influence (such as landfall).
Hurricanes also are a response to the global climate in which
they develop and can feed back to influence and perhaps even
change that climate. For example a series of hurricanes moving
into the higher latitudes in the Pacific can set off a train of
events that are still affecting European weather a year later.
From a societal perspective they are the most dangerous and
deadly of all natural atmospheric systems, capable of causing
widespread destruction and long-term disruptions to entire
societies. The damage wreaked by Katrina in New Orleans provides
a canonical example, but this was by no means the worse cyclone
in history. Even lesser damage on a small island nation can be
much more catastrophic and exceed their entire gross domestic
product. This capacity for disruption arises from three main
mechanisms: the high surface winds, the response of the ocean to
these winds, and the intense rainfall. These have widely
different contributions in different storms: the extended region
of high winds and particularly the storm-surge response were
dominant factors in Katrina; whereas the $>$10,000 deaths by
Hurricane Mitch arose entirely from rainfall and the associated
flooding and landslides. Societal response to this danger
involves complex interplays of warning, communication culture,
previous experiences and perceptions, interplays that are neither
well understood nor adequately predictable.
To cite this abstract, use the following reference: http://meetings.aps.org/link/BAPS.2008.MAR.H6.1