Figure 7B-4 shows that the highest water level heights were in the New York harbor region near Edison, NJ. The maximum height plotted was ______ ft. These occurred generally near the area where wind gusts and presumably average speeds were highest. a.6.5 b.8.9 c.11.5
Figure 7B-4 shows that the highest water level heights were in the New York harbor region near Edison, NJ. The maximum height plotted was ______ ft. These occurred generally near the area where wind gusts and presumably average speeds were highest. a.6.5 b.8.9 c.11.5
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
Related questions
Question
100%
Figure 7B-4 shows that the highest water level heights were in the New York harbor region near Edison, NJ. The maximum height plotted was ______ ft. These occurred generally near the area where wind gusts and presumably average speeds were highest.
a.6.5
b.8.9
c.11.5
![Storm Surge Impacts in Coastal Regions
The most serious threat to the coastal zone from a hurricane or tropical storm is the storm surge. Storm surge is a dome of ocean water that travels with the hurricane,
from the eye to the right of the track in the Northern Hemisphere (where onshore winds are strongest). The low air pressure near the hurricane eye causes sea level to rise
about 0.5 m (1.6 ft.) for every 50-millibar drop in air pressure. Wind-driven water topped by waves also pushes forward on the right side of the path of the storm. Sea
level fluctuations caused by the astronomical tides can add or subtract to the surge height. These factors combine to generate a storm surge that can range in height from 1
m (4 ft.) for a weak hurricane to more than 6 m (18 ft.) for a particularly intense system.
As the storm nears shore, the ocean floor topography also becomes a factor. The volume of oncoming water may be negligible over a deep-ocean floor but becomes
monumental over a gently sloping, shallow floor. The density of water is 1000 kg/cm³. That is one metric ton of mass per cubic meter that, in a typical surge, might hit the
shore at speeds of 15-25 km per hr (9–16 mph). And this surge dome may extend 40 km (25 mi.) or more along the shore, making for millions of cubic meters of water.
The impact on coastal features, buildings, and roads can be catastrophic.
Figure 7B-4 is a map of selected observations of coastal inundation, or the height of water above ground level in feet, for Hurricane/Superstorm Sandy. The map was
compiled from U.S. Geological Survey and National Ocean Service gauge data as well as damage reports.
Poughkeepsie
5.1
Connecticut
Rhode Island
4.2
Westerly
New Haven
5.2
5.5
4.9 3.8
4.5
4.5
3.4Stamford
3.4 4.5
New Jersey
Riverhead
Bronx
3.7
Islip
3.9
3.4 3.1
4.3 5.6
Hempsted
5,5
Brooklyh
5.7
4.3 4.6
uOs pa
8.9
5.5
4.1
Inundation (ft)
less than 3 ft.
• 3 to 4 ft.
• 4 to 5 fL.
• 5 to 6 t.
• 6 to 7 ft.
7 to 8 ft.
greater than 8 ft.
Toms River
4.4
4.1
4.9 4.3](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2F4075dd7b-7cf0-4080-a9ab-c20ff4793850%2Ff51bc2e5-8d88-4821-9f65-a3dec4d8b03f%2F201tkt_processed.png&w=3840&q=75)
Transcribed Image Text:Storm Surge Impacts in Coastal Regions
The most serious threat to the coastal zone from a hurricane or tropical storm is the storm surge. Storm surge is a dome of ocean water that travels with the hurricane,
from the eye to the right of the track in the Northern Hemisphere (where onshore winds are strongest). The low air pressure near the hurricane eye causes sea level to rise
about 0.5 m (1.6 ft.) for every 50-millibar drop in air pressure. Wind-driven water topped by waves also pushes forward on the right side of the path of the storm. Sea
level fluctuations caused by the astronomical tides can add or subtract to the surge height. These factors combine to generate a storm surge that can range in height from 1
m (4 ft.) for a weak hurricane to more than 6 m (18 ft.) for a particularly intense system.
As the storm nears shore, the ocean floor topography also becomes a factor. The volume of oncoming water may be negligible over a deep-ocean floor but becomes
monumental over a gently sloping, shallow floor. The density of water is 1000 kg/cm³. That is one metric ton of mass per cubic meter that, in a typical surge, might hit the
shore at speeds of 15-25 km per hr (9–16 mph). And this surge dome may extend 40 km (25 mi.) or more along the shore, making for millions of cubic meters of water.
The impact on coastal features, buildings, and roads can be catastrophic.
Figure 7B-4 is a map of selected observations of coastal inundation, or the height of water above ground level in feet, for Hurricane/Superstorm Sandy. The map was
compiled from U.S. Geological Survey and National Ocean Service gauge data as well as damage reports.
Poughkeepsie
5.1
Connecticut
Rhode Island
4.2
Westerly
New Haven
5.2
5.5
4.9 3.8
4.5
4.5
3.4Stamford
3.4 4.5
New Jersey
Riverhead
Bronx
3.7
Islip
3.9
3.4 3.1
4.3 5.6
Hempsted
5,5
Brooklyh
5.7
4.3 4.6
uOs pa
8.9
5.5
4.1
Inundation (ft)
less than 3 ft.
• 3 to 4 ft.
• 4 to 5 fL.
• 5 to 6 t.
• 6 to 7 ft.
7 to 8 ft.
greater than 8 ft.
Toms River
4.4
4.1
4.9 4.3
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