Climate Signals
A slow-moving storm system, fed by unusually warm seas in the Gulf of Mexico, began on August 7 to unleash heavy rains in the Southeastern United States.
From Tuesday, August 9 through Sunday, August 14 the storm inundated Louisiana, Mississippi, Alabama, Florida and Texas, killing three people.
Five cities in Louisiana have reported rainfall totals of over two feet.
On August 11, a measure of atmospheric moisture, precipitable water, was in historic territory at 2.78 inches, a measurement higher than during some past hurricanes in the region.
Increased moisture in the air and unusually heavy rainfall are classic signals of climate change.
As the world warms, storms are able to feed on warmer ocean waters, and the air is able to hold and dump more water.
These trends have led to a pronounced increase in intense rainfall events and an increase in flooding risk.
In the Southeastern US, extreme precipitation has increased 27 percent from 1958 to 2012.
Southeastern US sees extreme rainfall, a classic signal of climate change
Beginning Sunday, August 7, a slow moving storm system headed northward
from the superheated Gulf of Mexico and unleashed heavy rains on the
Southeastern US, first targeting Florida's panhandle and northwestern
coast.
Perry, Florida, saw 4.5 inches of rain in just two hours on August 8,
and Hatch Bend, Florida, reported up to 12.4 inches of rain from Sunday
until 9am on Monday.
[1]
From Tuesday, August 9 through Sunday, August 14, the slow-moving storm
inundated Louisiana, Mississippi, Alabama, Florida and Texas, killing at
least three people.
[2]
Five cities in Louisiana have reported over two feet of rain, with Watson, Louisiana, topping the list at 31.39 inches.
[3]
The town of Lafayette, in the heart of the wettest part of the storm,
reported 10.39 inches of rain on Friday, setting the town's record of
wettest day until Saturday topped that at 10.40 inches.
[4]
Record flooding has been observed on at nine river gauges in Louisiana.
[12]
One of the clearest changes in weather globally and across the United States is the increasing frequency of heavy rain.
[5]
A warmer atmosphere holds more water vapor. And like a bigger bucket, a warmer atmosphere dumps more water when it rains.
The storm in the Southeastern US was supercharged by running over a
warmer ocean and through an atmosphere made wetter by global warming.
Climate change is now responsible for 17 percent of moderate extreme rainfall events, i.e. one-in-a-thousand
day events.
[6]
The more extreme the event, the more likely climate change was
responsible, as climate change affects the frequency of the extreme
events the most. In the instance of a one-in-a-thousand
year event, the odds that climate change was responsible is dramatically higher.
[6]
High sea surface temperatures feed moisture and energy into storms
The storm system was fed by moist winds coming off the Gulf coast
where sea surface temperatures are running hot, bumped up by global
warming.
On August 7, sea surface temperatures in the Gulf hovered
near 90°F (32°C) at temperatures 3.6°F-5.4°F (2-3°C) above average.
[7][8]
Along the central Gulf Coast, a measure of atmospheric moisture (from
the surface up to the jet stream level) known as precipitable water is
in the top percentile of historical values (3 to 3.5 standard deviations
above normal).
[9]
In
New Orleans, the precipitable water was determined to be 2.78 inches
Wednesday, which ranks among the top-five highest levels on record in
August.
[10]
As the world warms, storms are able to feed on warmer ocean waters, and the air is able to hold and dump more water.
Extreme rains and floods are consistent with climate change trends
Over the past century the US has witnessed a 20 percent increase in
the amount of precipitation falling in the heaviest downpours, which has
dramatically increased the risk of flooding.
[5]
Since
the 1980s, a larger percentage of precipitation has come in the form of
intense single-day events, and nine of the top 10 years for extreme
one-day precipitation events have occurred since 1990.
[11]
In the Southeastern US, extreme precipitation has increased 27 percent from 1958 to 2012.
[5]
Discover how Climate Signals are related
This tree of climate signals illustrates factors that link this event to climate change.
This tree of
climate signals
is schematic only. It illustrates factors that link individual events
to climate change. The diagram does not quantify the relative strength
of each factor, nor does it illustrate the natural factors that often
shape extreme events, including natural variability and regular
circulation changes. For more information, read more about this event.
Greenhouse Gas Emissions
Greenhouse gases from human activities—mainly the burning of
fossil fuels like coal and gas—are likely responsible for all the
observed warming since 1950. The fundamental physics of heat trapping
greenhouse gases has been understood since the nineteenth century.
Scientists have understood since the late 1970s that humans—by
increasing the atmospheric concentration of greenhouse gases from 280
parts per million in preindustrial times to what is now over 400
ppm—have effectively wrapped the Earth in a thicker blanket, trapping
more of the Earth’s infrared energy close to the surface.
Global Warming
From 1880 to 2012, the Earth warmed by 1.5°F (0.85°C) reversing a
long term cooling trend. The physics behind the Earth’s temperature
imbalance is simple. Scientists first realized that gases in the
atmosphere cause a greenhouse effect in the 19th century and have known
since the late 1970s that humans are now driving this effect, trapping
more of the Earth’s infrared energy close to the surface through fossil
fuel emissions. The atmospheric concentration of greenhouse gases has
increased from 280 parts per million in preindustrial times to what is
now over 400 ppm.
Increased Sea Surface Temperature
The amount of heat absorbed by the oceans has surged in the past
few decades, contributing to more intense storms, sea level rise, sea
ice melt, storm surge flooding and widespread ecosystem change.
Increased Atmospheric Moisture
A warmer atmosphere holds more moisture—about 7 percent more per
1°C of warming—and scientists have already observed a four percent
increase in atmospheric moisture due to the air’s ability to hold more
moisture as it warms. Storms supplied by climate change with increasing
moisture are widely observed to produce heavier rain and snow. Increased
atmospheric moisture content may also affect the El Niño Southern
Oscillation, which is a major driver of interannual climate variability,
by intensifying regional precipitation variability, and associated
extreme precipitation and drought events. Research indicates that the
increase in atmospheric moisture is primarily due to human-caused
increases in greenhouse gases.
Increased Extreme Precipitation
Global warming leads to an increase in both ocean evaporation into
the atmosphere and the amount of water vapor the atmosphere can hold.
High levels of water vapor in the atmosphere in turn create conditions
more favorable for heavy precipitation in the form of intense rain and
snow storms.
Increased Flooding Risk
Heavy precipitation is contributing to increased flooding around
the world. Flooding is worsened by regional climate trends such as
increases in heavy rain and snow, early snowmelt, and increased seasonal
precipitation. Flooding is also affected by non-climatic factors such
as land development, deforestation, levee placement and local
topography, making it challenging to determine an overarching climate
signal in flood trends.
Gulf Storm August 2016
A slow-moving storm system, fed by unusually warm seas in the Gulf
of Mexico, began on August 7 to unleash heavy rains in the Southeastern
United States. From Tuesday, August 9 through Sunday, August 14 the
storm inundated Louisiana, Mississippi, Alabama, Florida and Texas,
killing three people. Five cities in Louisiana have reported rainfall
totals of over two feet. On August 11, a measure of atmospheric
moisture, precipitable water, was in historic territory at 2.78 inches, a
measurement higher than during some past hurricanes in the region.
Increased moisture in the air and unusually heavy rainfall are classic
signals of climate change. As the world warms, storms are able to feed
on warmer ocean waters, and the air is able to hold and dump more water.
These trends have led to a pronounced increase in intense rainfall
events and an increase in flooding risk. In the Southeastern US, extreme
precipitation has increased 27 percent from 1958 to 2012.
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