quiz 5 (end of extratropical cyclones and chapter 4) Flashcards
How does Convergence win the race?
- storms intensify as ….
- Does this keep going on until the world is consumed in a giant storm?
- Recall that storms intensify as the trough and ridge in the upper atmosphere build via feedback from the storm
- this will not go on until the world is consumed in a giant storm because they are limited by environmental factors
The Dissipating Cyclone
1. how long does dissipation of a cyclone take
2. during this time what still happens
3. as cold air continues to move southeastward, what will happen to the trough
4. the low at the surface is directly underneath ___
- Dissipation of the cyclone can take several days to over a week depending on the maximum intensity of the storm
- During this time, active weather still occurs along the frontal boundary
- As cold air continues to move southeastward, the upper-level trough
will continue to deepen and will eventually cut off from the main
flow
- This “cutoff low” aloft has cold air in the center - The low at the surface is directly underneath the cutoff low aloft,
and the whole system slowly spin down as frictional convergence raises the pressure of the surface low
- Similar to dissipation of hurricane over land
The dissipating cyclone: Divergence and the Cutoff Low
1. How does the upper-level divergence change as the flow changes
from an upper level trough and ridge pattern to a cutoff low pattern?
Recall that divergence in the Jet stream is due to changes in flow curvature.
* No change in flow curvature from
counterclockwise (trough) to clockwise ridge)
anymore – always counterclockwise
* Divergence becomes insignificant
* Convergence wins and low
dissipate
- is there a change in flow curvature from counterclockwise (trough) to clockwise (ridge)? why?
- what does divergence become?
- surface low pressure systems are the result of….
- No change in flow curvature from counterclockwise (trough) to clockwise (ridge) anymore – always counterclockwise.
- This because wind is faster around the ridge than the trough - Divergence becomes insignificant
- With no change in wind speed, little divergence - Recall that surface low pressure systems are the result of net divergence.
- Convergence wins and low dissipates
- That is divergent flow aloft is greater than the convergent flow at the surface
True or false: You would expect a low pressure center to form or intensify at the surface when divergence is greater than convergence in a column of the
atmosphere
True
- When divergence aloft (in the upper atmosphere) is greater than convergence at the surface, air is being removed from the upper levels faster than it’s being replaced from below. This creates a net upward motion of air, which leads to lower surface pressure
Extratropical Cyclones in North America
- cyclones preferentially form in five locations in North America (5)
- East of the Rocky Mountains
- East of Canadian Rockies
- Gulf Coast of the US
- East Coast of the US
- Bering Sea & Gulf of Alask
Origins of the Coastal Cyclones
1.coastal cyclones form in two regions
2. why are the cyclones along the East and Gulf Coasts often more intense than the Rocky Mountain counterparts
- Costal cyclones form in two regions: (1) off the central East Coast and (2) off the Gulf Coast
- Cyclones form along the East and Gulf Coasts of the US are often more intense than their Rocky Mountain counterparts, because of:
Coastal cyclones form over warm water = more latent heat to cyclones
More sensible heat from ocean to
cyclone
Stronger thermal contrast btw land and ocean
Exist both the polar and subtropical
jetstreams
Cyclones over water experience less
friction
- Cyclones form along the East and Gulf Coasts of the US are often more intense than their Rocky Mountain counterparts, because of:
How Often are the Coastal Cyclones?
- what effect do coastal cyclone shave on the northeast US and Canada
- how often and what seasons
- Coastal cyclones have the greatest economic impact of any storm type on the northeast United States and Canada, even more than hurricanes.
- Extratropical cyclones form along the East and Gulf Coasts of North America several time each year during late fall, winter, and early spring
EXTREME WEATHER AND THE AMERICAN REVOLUTION
- The Winter of 1779-80
- The Great Hurricane of 1780
- The Battle of Trenton
- Extreme weather significantly impacted the American Revolutionary War, both on the battlefield and for civilians. Notable events
- The Winter of 1779-80: This winter, considered the coldest on record for the East Coast, severely tested the
Continental Army, particularly during their winter quarters outside Morristown, New Jersey. Snowstorms, including a blizzard that dumped four feet of snow, left soldiers lacking essential supplies like coats, shoes, and food. - The Great Hurricane of 1780: This devastating hurricane caused significant losses to both the British and French navies, which were using Caribbean ports as staging areas. The storm contributed to the French deciding to move their ships north, which ultimately aided the American forces at the Siege of Yorktown.
- The Battle of Trenton: On December 25, 1776, George Washington led his troops across the icy Delaware
River. During the crossing, weather conditions worsened, with sleet and snow hindering their progress
A Little Rhode Island History and Weather
- 1776- British occupied Newport
- During the “Little Ice Age”
- Not a true ice age of global extent.
- Unusually cold time, defined as extending from the 16th to the 19th
centuries. - British burned about half of Newport for firewood to stay warm
- Almost half of the town evacuated. Didn’t recover from the economic
effect until mid 1800’s. - Industrial revolution didn’t take off there as it did in other American
cities. No pressure to tear down the colonial buildings. This is why
Newport has more colonial buildings than any other American city
Battle of Rhode Island
- 1778- French join war and bring war ships and troops into Narragansett Bay to help drive English out of Newport.
- English Navy approaches the Bay. French don’t want to get trapped. Leave Bay to engage English.
- Large storm rolls in and damages and scatters both navies.
- Result- Battle of Rhode Island was a nothingburger.
battle of rhode island
- continued
- English abandoned Newport in October 1779, when the British, facing
strategic challenges elsewhere, decided to evacuate Rhode Island. - In July 1780, a French army, led by General Rochambeau, arrived in
Newport. The French troops, a significant force of over 5,000 men,
established a base in Newport and later played a key role in the American victory at Yorktown. - July 1781, the French force left Rhode Island and marched across
Connecticut to join Washington on the Hudson River in New York. - General’s Washington and Rochambeau then marched their combined forces to the siege of Yorktown and the Battle of the Chesapeake. Surrounded the British who surrendered
A Few Notable Nor-easters
1. hurricane sandy
2. halloween 2011
3. april 14 to 18, 2007
- Hurricane Sandy- October 2012- record-setting storm surge was responsible for an estimated $62 billion in damage and loss in the U.S., as well as $315 million and 71 deaths in the Caribbean. Just as the hurricane headed northward along the coast, leaving Florida for the Eastern Seaboard, a cold nor’easter, morphed it into a hybrid part nor’easter.
- Halloween 2011- nor’easter ushered in a white Halloween. Snow began
falling in record amounts on Oct. 29, 2011. About 3 million people who lived
in areas impacted by the storm were left without power for days, thanks to
power lines brought down by heavy ice and snow - April 14 to 18, 2007 portions of Connecticut, Maine, New Jersey, New York and New Hampshire flooded homes and businesses, as well as property damaged by high winds and travel made treacherous by snowfall
The massive storm system measured 800 miles (1,287 kilometers) across,
intensifying into a nor’easter and reaching from the Carolinas to Canada
The Blizzard of 1978
- The Blizzard of 1978- catastrophic,
nor’easter that struck New England,
New Jersey, Pennsylvania, and the
New York metropolitan area
Connecticut, Rhode Island, and
Massachusetts were hit especially hard
by this storm - Providence also broke a record with
27.6 inches (70 cm) of snow; Nearly
all economic activity was disrupted in
the worst-hit areas. The storm killed
about 100 people in the Northeast and
injured about 4,500. It caused more
than US$520 million (US$2.51 billion
in 2024 terms) in damage
Yearly Beach Cycle
- Summer
- Winter
Summer
- gentle waves
- carry sand to shore but too weak to carry back to sea
- wider beach results
Winter
- erosive storm waves
- sand carried seaward to offshore sandbars
- narrow beach
effects of hard structures on beach erosion
Hard structures tend to cause
more erosion
Beach Replenishment: Sand Pumped from offshore
- Process by which sediment, usually sand, lost through longshore drift or erosion is replaced from other sources.
- Nourishment is typically a repetitive
process since it does not remove the
physical forces that cause erosion but
simply mitigates their effects. - The first nourishment project in the
United States was at Coney Island, New
York in 1922 and 1923. It is now a
common shore protection measure used by public and private entities. - Since 1923, the U.S. has spent $9 billion to rebuild beaches
Review: Extratropical Cyclones in North
- Cyclones preferentially form in
five locations in North America:
(1) East of the Rocky Mountains
(2) East of Canadian Rockies
(3) Gulf Coast of the US
(4) East Coast of the US
(5) Bering Sea & Gulf of Alaska
east coast cyclone: prior to development
- east coast cyclones typically develop after ….
- the cold air damming between the coast and the appalachian mountain leads to
- prior to cyclone development what happens with subtropical jetstreams
- East coast cyclones typically
develop after an earlier cyclone
originates east of the Rockies and
progresses across the continent,
which brings cold airs to the East
Coast. - The cold air damming between the
coast and the Appalachian Mountain leads to the formation of a coastal front. - Prior to the cyclone development, subtropical jetstream moves northward to merge with the polar jetstream
east coast cyclone: initial development
- where do jetstreaks and subtropical jetstreams move
- the upper-level divergence associated with the jetstreaks induced…
- latent and sensible heat released from the ocean and helps with …
- strong winds and heavy snows lead to what
- east coast cyclones also known as
- The jetstreaks in the polar and
subtropical jetstreams move eastward
and are on top of the surface coastal
front. - The upper-level divergence
associated with the jetstreaks induced
upper-level divergence which then
begin the development of a low
pressure center on the surface.
*Latent and sensible heat releases from
the ocean help the development.
*The pressure can drop as much
as 30mb in 24 hours.
*Strong winds and heavy snows lead
to blizzard conditions. - East Coast cyclones are called
“Nor’easter”
Explosive Cyclogenesis Bomb
- what do meterologists use to describe the rapid deepening of a low pressure center
- if the central pressure drops 24 mb in 24 hours what is the cyclone called
- Meteorologists use “explosive cyclogenesis” to describe the rapid deepening of a low- pressure center during cyclone formation.
- If the central pressure drops 24 mb in
24 hours, the cyclone is called a “bomb
cyclone”
east coast cyclone: mature phase
- east coast cylones track which way along the coast? when do they typically reach their maximum intensity?
- during this phase of the cyclone, the polar and subtropical jetstreams do what?
- what does the upper-level trough do
- a cutoff low is formed and what happens?
- the filling is slower over ____ than land
- East Coast cyclones track northeast
along the coast and typically reach
their maximum intensity 24-48
hours after the initial development.
*During this phase of the cyclone
evolution, the polar and subtropical jetstreams typically merge and
propagate northeastward along the
east side of the storm.
*The upper-level trough continues to
deepen and is eventually filled with cold air transported southward from west of the surface low.
*A cutoff low is formed and eventually filled by the convergence due to surface friction.
*The filling is slower over ocean
than over land.
Gulf Coast Cyclones
- when do gulf coast cyclones develop most frequently
- when do subtropical jetstreams tend to be strong
- gulf coast cycloes follow two tracks
Gulf Coast cyclones develop most
frequently during years when the
subtropical jetstream is a persistent
feature in the upper troposphere over
northern Mexico and the Gulf of
Mexico.
* Subtropical jetstreams tend to be
strong in El Nino years, therefore,
Gulf Coast cyclones are more
common during El Nino years.
* Gulf Coast cyclones follow two
tracks: (1) along the Gulf Coast and
then northeast along the Atlantic
Seaboard and (2) inland along the
Mississippi and Ohio River Valleys
El Nino and La Nina
- An important atmospheric variation that has an average period of three to seven years.
- Goes between El Nino, Neutral, and La Nina (ENSO cycle, El Nino Southern Oscillation)
- Has large influence both in the tropics and midlatitudes