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Earth is fighting to stay alive. Mass dieoffs, triggered by anthropogenic assault and fallout of planetary defense systems offsetting the impact, could begin anytime!

Posts Tagged ‘northern hemisphere’

Anthropogenic Hell Melting Icebox

Posted by feww on September 13, 2012

IF YOU WRECKED A HOLIDAY INN MOTEL ROOM , YOU’D PROBABLY GO TO JAIL.

Northern Hemisphere Ice Cover Continues Shrinking

The Arctic Sea Ice Extent shrank to 3.46 million square kilometers (3,456,695.22 km²) on September 12, 2012, according to National Snow and Ice Data Center (NSIDC).

 


Multi sensor Analyzed Sea Ice Extent – Northern Hemisphere (MASIE -NH), September 11, 2012.  Source: The National Snow and Ice Data Center (NSIDC)

Northern Hemisphere ice cover (million km²). Center for Ocean and Ice, Danish Meteorological Institute


Original Caption: The total area of sea ice is the sum of First Year Ice (FYI), Multi Year Ice (MYI) and the area of ambiguous ice types, from the OSISAF ice type product. However, the total estimated ice area is underestimated due to unclassified coastal regions where mixed land/sea pixels confuse the applied ice type algorithm. The shown sea ice extent values are therefore recommended be used qualitatively in relation to ice extent values from other years shown in the figure. In late 2012 sea ice climatology and anomaly data will be available here.

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Global Disasters: Links, Forecasts and Background

GLOBAL WARNING

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Image of the Day: ASIE

Posted by feww on September 7, 2012

Northern Hemisphere Ice Cover falls below 3.6 million km² —FIRE-EARTH 

As of September 5, 2011, the Arctic sea ice extent (ASIE) was 3,686,199.43 km² according to NSIDC.

  • Daily average ice melt for September currently stands at more than 87,000 km², NSIDC data shows.

Arctic sea ice extent fell below 3.6 million square kilometers (1.39 million square miles) on September 6, 2012, FIRE-EARTH estimates.

FEWW model shows the Arctic sea ice extent could fall to about 3 million km² (1.15 million square miles) during the 2012 melt season with a probability of 0.5 [P = 54%]


Multi sensor Analyzed Sea Ice Extent – Northern Hemisphere (MASIE -NH), September 5, 2012.  Source: The National Snow and Ice Data Center (NSIDC)

Related Links

Global Disasters: Links, Forecasts and Background

GLOBAL WARNING

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Arctic Sea Ice Extent Could Fall to 3M Km²

Posted by feww on September 3, 2012

UPDATED September 4, 2012 @ 01:44UTC

Northern Hemisphere Sea Ice Cover Shrinking Rapidly

Arctic sea ice extent shrank to about 3.65 million square kilometers (1.41 million square miles) on September 2, 2012, FIRE-EARTH estimates.

FEWW model shows the Arctic sea ice extent could fall to about 3 million km² (1.15 million square miles) during the 2012 melt season with a probability of 0.5 [P = 54%]


Arctic sea ice extent as of September 1, 2012.  Image Source: NSIDC


Arctic sea ice extent, September 1, 2012. FIRE-EARTH estimates the NH ice cover fell below 3.65 million km² (1.41 million square miles) on September 2, 2012.
  Image Source: NSIDC

Arctic Sea Ice Cover:  Denmark’s Center for Ocean and Ice (DMI)


Original caption:  Current Sea Ice extent. Total sea ice extent on the northern hemisphere since 2005. The ice extent values are calculated from the ice type data from the Ocean and Sea Ice, Satellite Application Facility (OSISAF), where areas with ice concentration higher than 30% are classified as ice.        The total area of sea ice is the sum of First Year Ice (FYI), Multi Year Ice (MYI) and the area of ambiguous ice types, from the OSISAF ice type product. However, the total estimated ice area is underestimated due to unclassified coastal regions where mixed land/sea pixels confuse the applied ice type algorithm. The shown sea ice extent values are therefore recommended be used qualitatively in relation to ice extent values from other years shown in the figure.

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Global Disasters: Links, Forecasts and Background

GLOBAL WARNING

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Arctic Sea Ice Extent Down to 3.87M km² and Melting

Posted by feww on August 31, 2012

Northern Hemisphere Sea Ice Cover Continues Shrinking

Arctic sea ice extent shrank to about 3.87 million square kilometers (1.49 million square miles) on August 29, 2012 and continued melting, FIRE-EARTH estimates. The new record low was 100,000 km² below the September 18, 2007 daily extent of 4.17 million km².

FEWW model shows the Arctic sea ice extent could fall below 3.8 million km² during the 2012 melt season with a probability of 0.8 [P≥77%]


Arctic sea ice extent, August 29, 2012. FIRE-EARTH estimates the NH ice cover has fallen below 3.87 million km².  Image Source: NSIDC


Arctic sea ice extent as of August 29, 2012. The ice extents is now the lowest in the satellite record.  Image Source: NSIDC

Related Links

Global Disasters: Links, Forecasts and Background

GLOBAL WARNING

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Arctic Sea Ice Extent Breaks Record Low and Melting

Posted by feww on August 28, 2012

Northern Hemisphere Sea Ice Cover Falls to Record Low

Arctic sea ice extent shrank to 4.10 million square kilometers (1.58 million square miles) on August 26, 2012 and continued melting. The new record low was 70,000 km² below the September 18, 2007 daily extent of 4.17 million km², National Snow and Ice Data Center (NSIDC) reported.

FEWW model shows the Arctic sea ice extent could fall below 3.8 million km² during the 2012 melt season with a probability of 0.7 [P≥72%]


Arctic sea ice extent as of August 26, 2012, along with daily ice extent data for 2007, the previous record low year, and 1980, the record high year. The six lowest ice extents in the satellite record have occurred in the last six years (2007 to 2012). Source: NSIDC


Arctic sea ice extent for September 18, 2007, daily extent of 4.17 million km², and August 26, 2012 (right), 4.10 million km².  Source: NSIDC

[Note: NSIDC  has changed the date and extent of the 2007 minimum to September 18, 2007 and daily extent of 4.17 million km² from the previous figure of 4.28 million km²]

Global Disasters: Links, Forecasts and Background

GLOBAL WARNING

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Arctic Ice Affects Global Climate, Weather

Posted by feww on March 17, 2010

Arctic ice-melt is not just a local issue, it affects climate, weather globally

Melting sea ice may appear to be  or local at worst regional problem, but NOAA says that changes in the Arctic ice cover also influence weather in the mid-latitudes, where the majority of humans live.


Satellite images show a clear acceleration in the Arctic ice loss for the past 30 years.  For additional information visit
Will the Arctic be free of summer ice in 30 years?

Just about every model available for the Arctic ice cover in the future predict a continuation of the present pattern, an acceleration in the ice melt.

What happens when the open arctic waters absorb the additional heat?


The additional heat impacts the Arctic winds and therefore the Arctic atmosphere, increasing the variability and unpredictability of global wind patterns. For additional information visit How the loss of sea ice leads to a warmer Arctic

Cold arctic winds move to mid-altitude regions of the globe, spawning violent winter storm in the U.S. and Eurasia.

Teleconnections impact mid-latitudes

Warmer temperatures that result from huge losses in the sea ice cover give rise to higher pressure surfaces above the North Pole which in turn impact large scale wind patterns over the Northern Hemisphere. “Climate models show these connections with cold air moving south, producing low pressure areas and unusually cold winters in the eastern U.S. and eastern Asia, and cooler than usual weather in late winter from Europe to the Far East.”  For additional information visit How changes in the Arctic impact weather and climate in Europe, Asia and the US.

See also:  Transitory Impact of AO is the ‘Good News’

How much warmer is the Arctic?

In the figures below, red, yellow and green colors indicate areas over the Arctic region where autumn near-surface air temperatures were from 2 to 6°C warmer than the normal values observed prior to 2002.


Anomalies for autumn in 2002-2005 represent deviations from the normal near surface air temperature values which were observed from 1968-1996. Figure from Overland and Wang via NOAA

Anomalies for autumn 2007-2008 represent deviations from the normal near surface air temperature values which were observed from 1968-1996. Figure from Overland and Wang via NOAA


Anomalies (above) represent deviations from normal pressure surface elevations over the Arctic. Figure from Overland and Wang via NOAA

Warmer Arctic changes the Arctic atmosphere, impacts global winds

The elevated pressure surfaces above the North Pole persist into early winter and impact large scale wind patterns over the Northern Hemisphere, allowing cold are to move southward.

Figure (below) shows the changes in the Northern Hemisphere wind fields that are associated with late autumn surface air temperature and earlier sea loss. Blue and purple colors indicate areas with wind deviations below normal. Note the much reduced winds north of Alaska and western Canada.2

The reduction in winds opposes the usual atmospheric circulation patterns, allowing outbreaks of cold Arctic air to move southward.

It must be noted that there is considerable year-to-year variability in pressure fields, and that modifications of mid-latitude weather by wind patterns associated with sea ice reduction can be complex (involving storm track and longwave interactions).

However a consequence of the changes in Arctic atmospheric temperature and pressure, following loss of sea ice, is increased likelihood of cold air moving southward via teleconnections to impact weather at mid-latitudes.

As summer Arctic open water area increases over the next decades, we anticipate an increasing influence of loss of summer sea ice on the atmospheric northern hemisphere general circulation in following seasons with resultant impacts on northern hemisphere weather. For more information visit source: Loss of summer Arctic sea ice … and  Arctic Future Web site


Anomalies (above) represent deviations from normal east-west winds over the Arctic. Figure from Overland and Wang via NOAA

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Posted in Arctic winds, Climate Change, Eurasia winter, Teleconnections, US weather | Tagged: , , , , , , | 1 Comment »

Transitory Impact of AO is the ‘Good News’

Posted by feww on January 9, 2010

The Bad News?
More Permanent Changes May Be Occurring!

Impact of Arctic Oscillation on Winter Temps

[Stay Tuned …]


Click image to enlarge.
See  Kingdom United by Ice for detailed data and charts. Image Credit: NASA EO.

NASA image compares December 2009 temps to the average December temps between 2000 and 2008. Blue (red) for colder (warmer) than average land surface temps.

The Arctic Oscillation (AO), a climate pattern, impacts  winter weather in the Northern Hemisphere. The Arctic is dominated by a low-pressure air mass, while the mid-latitudes (around 45 degrees North, about the latitude of Montreal, Canada or Bordeaux, France) are governed by high pressure systems.

The strength of the high- and low-pressure systems oscillates. Weaker than normal systems cause the pressure difference between the two to decrease, allowing Arctic air to escape south and warmer air north. A weaker-than-normal AO is defined as “negative.” Strong high and low pressure systems characterize positive AO.

AO was strongly negative during Dec 2009. This image  observed by MODIS on NASA’s Terra satellite shows cold Arctic air impacting land surface at midlatitudes, while Arctic land, like Greenland and Alaska, was much warmer than usual. NASA Earth Observatory image by Kevin Ward. Caption by Holli Riebeek. Edited by FEWW.

See    Kingdom United by Ice for detailed data and charts

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Posted in AO, Arctic weather, Icebox weather, Negative Arctic Oscillation, Winter Temps | Tagged: , , , , | 8 Comments »

United Kingdom of Ice

Posted by feww on January 8, 2010

Arctic Oscillation in Strong Negative Phase:
Why Northern Hemisphere is So Cold

Image of the Day: United Kingdom, Where the Ice Never Thawed!


Photo Credit: NASA/ MODIS Rapid Response. Click Image to enlarge.

Arctic Oscillation (AO)

The loading pattern of the AO is defined as the leading mode of Empirical Orthogonal Function (EOF) analysis of monthly mean 1000mb height during 1979-2000 period.

Arctic Oscillation Loading Pattern
Click image to enlarge.

The negative phase of the Arctic Oscillation (AO) has been a contributing factor to the arctic cold weather and blanket snow at the mid-latitudes across much of Northern Hemisphere since December 2009. The Arctic Oscillation Index in December 2009 fell to its lowest monthly value since 1950.

Observed Daily Arctic Oscillation Index.
Click image to enlarge.
The daily AO index is constructed by projecting the daily (00UTC) 1000mb height anomalies poleward of 20°N onto the loading pattern of the AO.  Year-round monthly mean anomaly data has been used to obtain the loading pattern of the AO (Methodology).  Since the AO has the largest variability during the cold season, the loading pattern primarily captures characteristics of the cold season AO pattern. Source: NOAA/ National Weather Service

Vertical Cross section of Geopotential Height Anomalies and AO index. Click on image to enlarge.
Click image to enlarge.
The daily geopotential height anomalies at 17 pressure levels are shown for the previous 120 days as indicated, and they are normalized by standard deviation using 1979-2000 base period. The anomalies are calculated by subtracting 1979-2000 daily climatology, and then averaged over the polar cap poleward of 65°N.

The blue (red) colors represent a strong (weak) polar vortex. The black solid lines show the zero anomalies.  Source: NOAA/  National Weather Service


Click image to enlarge.
The standardized 3-month running mean value of the AO index. The departures are standardized using the 1950-2000 base period statistics.  Source: NOAA/  National Weather Service

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Posted in AO negative phase, Arctic Oscillation, cold season AO pattern, polar vortex, treme cold | Tagged: , , , , | 9 Comments »

Tropical Cyclones

Posted by feww on May 6, 2008

What’s a Tropical cyclone?

A tropical cyclone is a storm system characterized by a low pressure center and numerous thunderstorms that produce strong winds and flooding rain. A tropical cyclone feeds on the heat released when moist air rises and the water vapor it contains condenses.

The term “tropical” refers to both the geographic origin of these systems, which form almost exclusively in tropical regions of the globe, and their formation in Maritime Tropical air masses. The term “cyclone” refers to such storms’ cyclonic nature, with counterclockwise rotation in the Northern Hemisphere and clockwise rotation in the Southern Hemisphere. Depending on their location and strength, tropical cyclones are referred to by other names, such as hurricane, typhoon, tropical storm, cyclonic storm, tropical depression and simply cyclone.


Map of the cumulative tracks of all tropical cyclones during the 1985–2005 time period.

Tropical cyclones can produce extremely powerful winds and torrential rain, as well as high waves and devastating storm surge. They develop over large bodies of warm water, and can cause significant damage to coastal regions flooding up to 40km from the coastline. Although inland regions are relatively safe from receiving strong winds, heavy rains can produce significant flooding inland. (Source)

Cyclones can relieve drought conditions

Known for devastating human populations, tropical cyclones can also relieve drought conditions. They also carry heat and energy away from the tropics and transport it towards temperate latitudes, which makes them an important part of the global atmospheric circulation mechanism. As a result, tropical cyclones help to maintain equilibrium in the Earth’s troposphere, and to maintain a relatively stable and warm temperature worldwide. (Source)


Structure of a tropical cyclone (Source: NOAA)

Cyclone Structure

Tropical cyclones are areas of low atmospheric pressure near the Earth’s surface. The pressures recorded at the centers of tropical cyclones are very low. Tropical cyclones are driven by the release of large amounts of latent heat of condensation, which occurs when moist air is carried upwards and its water vapor condenses.

Eye and inner core

A strong tropical cyclone will harbor an area of sinking air at the center of circulation. If this area is strong enough, it can develop into an eye. Weather in the eye is normally calm and free of clouds, although the sea may be extremely violent. The eye is normally circular in shape, and may range in size from 3 km to 370km in diameter. (Source)

Brief History:

The 1970 Bhola cyclone is the deadliest tropical cyclone on record, killing more than 300,000 people and potentially as many as 1 million after striking the densely populated Ganges Delta region of Bangladesh on November 13, 1970. Its powerful storm surge was responsible for the high death toll. The North Indian cyclone basin has historically been the deadliest basin, with several cyclones since 1900 killing more than 100,000 people, all in Bangladesh. Super Typhoon Nina caused major damage and deaths in China, mainly from the collapse of the Banqiao Dam. Hundreds of thousands of people died due to the resulting floods, making it one of the deadliest tropical cyclones recorded in history. The collapse of the dam due to heavy floods also caused a string of 60 or so smaller dams to collapse. (Source)

Global Warming and Hurricanes

Source: Geophysical Fluid Dynamics Laboratory

The strongest hurricanes in the present climate may be upstaged by even more intense hurricanes over the next century as the earth’s climate is warmed by increasing levels of greenhouse gases in the atmosphere. […]
According to a new simulation study by a group of scientists at NOAA’s Geophysical Fluid Dynamics Laboratory (GFDL), a 5-12% increase in wind speeds for the strongest hurricanes (typhoons) in the northwest tropical Pacific is projected if tropical sea surfaces warm by a little over 2°C (Figure 1). Recent preliminary findings indicate that these results may apply to the other tropical cyclone basins as well. […] (Source: OAR NOAA)

Recent Cyclones and Hurricanes:

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Food: Worse times ahead

Posted by feww on May 4, 2008

Climate Change + Higher temperatures + Droughts + Floods + Soil erosion + Loss of topsoil + Pollution + Ground-level Ozone = Much Less Food in the Future

Scientists are warning that global warming would present great challenges on the way to produce more food in the future.

“There certainly are going to be lots of challenges in the future. Temperature is one of them, water is another,” said Lisa Ainsworth, a molecular biologist with the United States Department of Agriculture.

“In Northeastern China, low temperatures, a short growing season and lack of water limit production, so rising temperatures in the future may have beneficial impacts there,” said Ainsworth.

“However, in the southern parts of the country, higher temperatures will likely cause yield losses,” she told the reporters.

Higher temperatures coupled with ground-level ozone, which is produced as a result of sunlight interacting with greenhouse gases, added to extremes of floods and droughts is a recipe for disaster.

Ozone is a growing problem in the northern hemisphere and is already costing farmers billion of dollars in crop damage.


Effect of increasing ozone concentration (left to right: about 15, 80 and 150 ppb) on growth of (A) Pima cotton and nutsedge grown in direct competition with one nutsedge per cotton; (B) tomato and nutsedge
grown in direct competition with nutsedge (two-to-one); and (C) yellow nutsedge grown in the absence of competition. (Photo and caption: David A. Grantz & Anil Shrestha, UC Kearney Agricultural Center )

“In the major rice-growing regions, which are India and China, ground-level ozone concentrations even today are very high and certainly exceed the threshold for damage. Ozone is already decreasing yield potential in many areas,” Ainsworth said.

Significant amounts of rice yield are lost annually due to various abiotic stresses (e.g., salinity, droughts). Rice is the staple diet for about half of the world population, and about 90 percent of the world’s rice is produced in Asia.

UN experts believe that in low-latitude regions, slightest temperature rises of about 1ºC could affect crop yields.

The atmospheric CO2 levels have now reached about 388 parts per million from about 280 ppm prior to the Industrial Revolution.

“There is still a lot of uncertainty in the climate modeling when it comes to the regional level,” said Reiner Wassmann coordinator of the Rice and Climate Change Consortium at IRRI. “But it was clear temperatures would rise.”


A train travels along the flooded Darbhanga-Sitamadhi railway line in Bihar in this August 2, 2007 file photo. Massive monsoon floods in eastern India damaged vast areas of corn and affected the rice crop, government officials and farm experts said on Tuesday, adding that losses are being assessed. REUTERS/Krishna Murari Kishan (image may be subject to copyright!) See FEWW Fair Use notice.

“The other mega trend we see is that we will have more climate extremes. In some places there might be more drought, in others it may be submergence, from floods, in some places it might be both,” said Wassmann.


Lake Hartwell, February 2008, western South Carolina. Photo courtesy South Carolina Department of Natural Resources staff. (Source UNL)

“That is really a new challenge for development of cropping systems and I don’t want to limit it to only plant breeding. We have to be clear that this is no silver bullet and that if we speed-up plant breeding everything will be fine. Certainly not.

“We also have to improve crop management and water saving techniques have come into the picture to cope with drought,” he said. (Source)

High ozone levels can damage leaves on trees and crops (such as corn, wheat, and soybeans), reducing growth rates and crop yields. In 1995, ground-level ozone caused $2.7 billion in crop damage nationwide, according to the U.S. Environmental Protection Agency. Due to its reactive nature, ozone also can prematurely degrade and wear out rubber, paints and other materials. (Source)

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Posted in Climate Change, environment, food, Global Warming, health, politics | Tagged: , , , , , , , , , , , , , , , , , , , , , , , , , | 5 Comments »