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Copyright © 2017 University of Maryland This material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 1 Tim Canty Class Web Site: http://www.atmos.umd.edu /~tcanty/aosc200 Lecture 25 Nov 28 2017 Tropical Cyclones: When Nature Attacks!! AOSC 200 Topics for today: Really powerful low pressure systems Copyright © 2017 University of Maryland This material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 2 Multi-vortex Tornado http://4.bp.blogspot.com/_R8xVtHAV1lc/SjnJ- KLIzfI/AAAAAAAABQ8/AQl94p6_s-w/s400/Tornado-multivortex.jpg

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Page 1: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 1

Tim Canty

Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200

Lecture 25Nov 28 2017

Tropical Cyclones: When Nature Attacks!!AOSC 200

Topics for today:

Really powerful low pressure systems

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 2

Multi-vortex Tornado

http://4.bp.blogspot.com/_R8xVtHAV1lc/SjnJ-KLIzfI/AAAAAAAABQ8/AQl94p6_s-w/s400/Tornado-multivortex.jpg

Page 2: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 3

Tornado Frequency

Fig 10-36 Essentials of Meteorology

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 4

Tornado Death Frequency

Fig 11-27 Meteorology: Understanding the Atmosphere

Page 3: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 5

Tropical Cyclone

Known by several names:

• Hurricanes – Atlantic Ocean, Eastern North Pacific• Typhoons – Pacific Ocean• Cyclones – Indian Ocean

Must have minimum wind speed of 74 mph and rotational circulation

“Major Hurricane” – Category 3 or higher“Super Typhoon” – Category 4 or higher

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 6

Tropical Cyclone: African Easterly Jet

Tropical Disturbance:

• Mid-level, Easterly winds blowing off of the hot Sahara

http://www.meted.ucar.edu/dynamics/thermal_wind/navmenu.php?tab=1&page=11.4.0&type=text

Saharan Air Layer

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Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 7

Tropical Cyclone: Life Cycle

Tropical Disturbance:

• Tropical weather system 100 to 300 nmi in diameter• Originates in tropics or subtropics• May be associated with perturbations in the wind field known as easterly waves.

http://www.aoml.noaa.gov/hrd/tcfaq/A4.html

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 8

Tropical Cyclone: Life Cycle

Tropical Depression:

• Maximum sustained surface wind speed up to 38 mph • Depressions have a closed circulation• Weak low pressure center ~1010 mb

http://www.aoml.noaa.gov/hrd/tcfaq/A5.html

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Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 9

Tropical Cyclone: Life Cycle

Tropical Storm:

• Maximum sustained surface wind speed 39 mph to 73 mph• Convection usually more concentrated near the center• Outer rainfall organizing into distinct bands• Central pressure ~1000 mb

http://www.aoml.noaa.gov/hrd/tcfaq/A5.html

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 10

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Page 6: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 11

Tropical Cyclone: Life Cycle

Hurricane:

• Winds equal or exceed 74 mph• Further designated by categories on Saffir-Simpson scale • Central pressure can drop very low (Hurricane Wilma 882 mb)

http://www.aoml.noaa.gov/hrd/tcfaq/A5.html

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 12

Saffir-Simpson Scale

Page 7: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 13

Tropical Cyclone: Life Cycle

Fig 8-30 Meteorology: Understanding the Atmosphere

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 14

Hurricanes: 1851–2012

Hurricane Season: June 1 – November 30

Page 8: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 15

Recurvature: the “C” shaped path of Hurricanes

http://www.wunderground.com/blog/BDAwx/archive.html?year=2010&month=07

Hurricanes track around the “ “When they turn North, Westerly jet stream pushes hurricanes to North-East

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 16

Tropical Cyclone: Life Cycle

Fig 8-32 Meteorology: Understanding the Atmosphere

Strongly affected by sea surface temperature

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Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 17

Tropical Cyclone: Role of SST

Fig 8-23 Meteorology: Understanding the Atmosphere

Need SST greater than 26.5°C (found in the tropics)Evaporation increases quickly with rising temperature

Latent heat provides energy to storm

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 18

Hurricane Season

Fig 11-6 Essentials of Meteorology

Page 10: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 19

Tropical Cyclone: Why no cyclones near the equator?

Fig 8-23 Meteorology: Understanding the Atmosphere

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 20

Tropical Cyclone: Role of Wind Shear

Wind shear can rip apart storms before they can coalesce into a cycloneWinds spread out release of latent heat over large area

http://www.wunderground.com/education/shear.asp

Page 11: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 21

Tropical Cyclone: End of the storm

Tropical Cyclones diminish when they

• move over cold ocean water

• move over land

• interact with aloft winds or pressure systems

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 22

Anatomy of a Hurricane

Fig 11-2 Essentials of Meteorology

Page 12: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 23

Anatomy of a Hurricane

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 24

Anatomy of a Hurricane

https://www.wunderground.com/blog/JeffMasters/comment.html?entrynum=3470&page=5

Aircraft observations of Hurricane Matthew

Page 13: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 25

Anatomy of a Hurricane

Fig 11-3 Essentials of Meteorology

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 26

Tropical Cyclone: Wind Damage

Hurricane winds can be increased or reduced along pathCan spin off tornadoes

Fig 11-16 Essentials of Meteorology

Winds on the right side blow in the same direction as the hurricane is moving. Add the two speeds together.

Winds on the left side blow in the opposite direction as the hurricane is moving. Subtract the two speeds.

Page 14: Class Web Site: …tcanty/aosc200/lectures/AOSC_200_2017_lectur… · Title: AOSC 200 Weather and Climate Author: Tim Canty Created Date: 11/28/2017 12:15:08 PM

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 27

Tropical Cyclone: Seawater

Ocean water “piles up” in front of storm due to winds and low pressure

http://www.nhc.noaa.gov/surge/

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 28

Tropical Cyclone: Seawater

Storm surge can combine with normal tidal variationsSurge can greatly erode beaches

http://www.nhc.noaa.gov/surge/

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Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 29

Tropical Cyclone: Rainfall

Doppler Radar of Tropical Storm AllisonWhite areas = 36 inches of total rainfall

Fig 8-36 Meteorology: Understanding the Atmosphere

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 30

Tropical Cyclone: Rainfall

Flooding after Hurricane Floyd, 1999

http://www.nws.noaa.gov/ohd/hurricane/inland_flooding.html

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Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 31

Hurricane Sandy

http://www.wunderground.com/blog/JeffMasters/comment.html?entrynum=2283

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 32

Hurricane Sandyy

Greene et al., Oceanography, 2014

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Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 33

Hurricane Sandy

Copyright © 2017 University of MarylandThis material may not be reproduced or redistributed, in whole or in part, without written permission from Tim Canty 34

Hurricane Sandy (landfall)

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Hurricane Isabel (Sept 14, 2003)

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Hurricane Isabel (Sept 14, 2003)

• Wind gusts in central Maryland peaked at 83 mph in Silver Spring

• Storm surge along Western Shore peaked at 8.2 ft in Baltimore.

• Annapolis reported a surge of 7.2 ft

• Total cost ~$1.2 billion