Tropical Cyclones - genesis depends on ocean conditions - huge removal of heat energy from ocean -...

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Transcript of Tropical Cyclones - genesis depends on ocean conditions - huge removal of heat energy from ocean -...

Page 1: Tropical Cyclones - genesis depends on ocean conditions - huge removal of heat energy from ocean - damage primarily from storm surge caused by strong.
Page 2: Tropical Cyclones - genesis depends on ocean conditions - huge removal of heat energy from ocean - damage primarily from storm surge caused by strong.

Tropical Cyclones

- genesis depends on ocean conditions

- huge removal of heat energy from ocean

- damage primarily from storm surge caused by strong winds

Geography 104 - “Physical Geography of the World’s Oceans”

Page 3: Tropical Cyclones - genesis depends on ocean conditions - huge removal of heat energy from ocean - damage primarily from storm surge caused by strong.
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High and Low Pressure Systems

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warm and cold fronts

general east-west movement following jet stream

cold front usually more intense

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largest most intense storm systems are not fronts, but huge rotating masses of low pressure known as tropical cyclones

paths taken by hurricanes, cyclones, and typhoons (following trade winds in east to west direction)

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Tracks of all tropical cyclones, 1985-2005Tracks of all tropical cyclones, 1985-2005

Source: Wikipedia

Page 8: Tropical Cyclones - genesis depends on ocean conditions - huge removal of heat energy from ocean - damage primarily from storm surge caused by strong.
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hurricane Katrina (2005)

“The energy in a single hurricane is greater than that generated by all energy sources in the United States over the last 20 years.”

Essentials of Oceanography Textbook

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hurricane structure

powered by the release of vast amounts of water’s latent heat (condensation)

hurricane process:1. low pressure system

2. moisture from ocean

3. warm moist air rises

4. heat from condensation

5. warm air rises further

6. surface pressure lowers

7. go to 2.

typical diameter < ~100 miles

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hurricane intensity scaletropical depression < 38 mphtropical storm 38 – 74 mphtropical cyclone (hurricane)

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MODIS Image of Hurricane Katrina

(28 Aug 2005 - 1700 UTC)

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track of hurricane Katrina

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MODIS Image of hurricane Rita – 21 Sept. 2005

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storm track: Hurricane Rita

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storm surge – hurricane Rita

21 Sept. 2005

26 Sept. 2005

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flooding from storm surge during Katrina

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http://modis.gsfc.nasa.gov/gallery/individual.php?db_date=2007-10-06

Typhoon Krosa: 1-8 October 2007

http://earth.esa.int/ew/cyclones/Typhoon_Krosa-oct07/

-18 killed on Taiwan- China evacuates 1.4 million in Zhejiang and Fujian provinces

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Sea Surface Temperature (SST) Anomaly and Atlantic Tropical Cyclone Counts (Mann & Emanuel, 2006)

- SST and Atlantic hurricanes on the recent increase due to climate change

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Atlantic Hurricane Tracks 2005 and 1933 (Landsea, 2007)

- increased Atlantic hurricane frequency from new observational technologies

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Number of Atlantic tropical cyclones that struck land versus number that stayed over the open ocean. The solid line is the 1900–2006 long-term mean of 9.2 per year. (Landsea, 2007)

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Percentage of all reported Atlantic tropical cyclones that struck land. (Landsea, 2007)

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QuikSCAT Satellite – a microwave radar for measuring surface winds

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Quickscat launch – 19 June 1999

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wind speed from Quickscat (ascending pass)

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wind speed from Quickscat (descending pass)

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Hurricanes Strongly Mix the Upper Ocean

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SST ChangeSST Change

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Hurricane Francis (2004); ocean profiles before and after

- huge removal of heat from the ocean

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Readings (Ocean and Atmosphere):Text Chapter 8 (pgs 138 – 163)Reader pgs. 51 - 61 Reader Maps pgs 200 - 204

Midterm on Wednesday 5 Nov 2008