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May 9, 2008

Runaway Runoff: The Problem of Urban Runoff

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Runaway Runoff

Pavement, buildings and other waterproof surfaces cover a large portion of the land in urban areas like metropolitan Chicago. That means rain water cannot soak into the ground. Instead, it gushes into storm drains that discharge directly to local rivers and streams.

About 55 percent of rainwater that falls on a city runs off (and in intensely urbanized locations such as the Loop, runoff approaches 100 percent); only 15 percent of rainfall sinks in to recharge groundwater supplies. The remaining 30 percent evaporates back into the atmosphere.

For comparison, only 10 percent of rain that falls on natural ground cover (forests, wetlands or other natural areas) runs off, and about 50 percent soaks into the ground.

As rainwater runs over city surfaces, it picks up pollutants encountered along the way -- soil, oil and grease from cars, pesticides and fertilizers, pet waste and much more. Not only do such pollutants harm fish and wildlife, they also degrade drinking water supplies and often require that recreational waterways be closed.

What can you do?
If you plan to replace a walkway, driveway or patio in your yard this spring, consider using water-permeable surfaces such as wood decks, spaced bricks or concrete lattice instead of solid concrete or asphalt. These surfaces allow water to soak through to the ground, thereby reducing runoff from your property and helping to replenish groundwater supplies.

March 1, 2008

Understanding the Weather: March 1, 2008

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Chicago Midway Airport Summary for February, 2008
Period of record: 1929-2008

Data provided courtesy of Chicago weather historian Frank Wachowski

Total snowfall 22.8", or 221 percent of normal (10.3")
Third-snowiest February on record

Most snowfall in February
1 1994 26.2"
2 1980 23.7"
3 2008 22.8"

Total precipitation (water content) 3.71"
Second-wettest February on record

Most precipitation in February
1 1997 6.76"
2 2008 3.71"

Sunshine in February was 40 percent of possible versus normal of 46 percent

February 26, 2008

Understanding the Weather: Feb. 26, 2008

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Chicago has a national reputation of being a snowy city, but many U.S. cities routinely receive much more than Chicago's winter average of 39 inches. Here are several cities whose seasonal snow total is at least twice as great as Chicago's:

324" Valdez, Alaska
137" Marquette, Michigan
116" Syracuse, New York
102" Lander, Wyoming
100" Flagstaff, Arizona
99" Juneau, Alaska
98" Muskegon, Michigan
93" Buffalo, New York
92" Rochester, New York
81" Duluth, Minnesota
79" Burlington, Vermont

Understanding the Weather: Feb. 26, 2008

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Chicago has a national reputation of being a snowy city, but many U.S. cities routinely receive much more than Chicago's winter average of 39 inches. Here are several cities whose seasonal snow total is at least twice as great as Chicago's:

324" Valdez, Alaska
137" Marquette, Michigan
116" Syracuse, New York
102" Lander, Wyoming
100" Flagstaff, Arizona
99" Juneau, Alaska
98" Muskegon, Michigan
93" Buffalo, New York
92" Rochester, New York
81" Duluth, Minnesota
79" Burlington, Vermont

February 6, 2008

Understanding the Weather: Feb. 6, 2008

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Chicago snow extremes in February
(1885-2007)

snowiest February ... 27.8" in 1896

biggest February snowstorm ... 13.4" Feb. 6-7, 1895

least snowy February ... 0.0" in 1987 and 1998

February 5, 2008

Understanding the Weather: Feb. 6, 2008

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Drizzle: Liquid precipitation composed of very small water droplets (0.001 to 0.020 inch in diameter) that appear almost to float while following air currents. Unlike fog, drizzle falls to the ground. It is erroneous to refer to very light rain as drizzle.

Drizzle, fog, mist: All three are composed of tiny water droplets that appear to float in the air. Drizzle droplets are large enough so that they do fall, and therefore drizzle is precipitation. Fog and mist droplets are smaller and do not fall and are not precipitation.

Fog: A visible aggregate of water droplets suspended in the air at ground level. Fog is literally a cloud on the ground. Fog droplets are so tiny that they do not fall through the air, and fog is therefore not considered to be precipitation.

Freezing rain: Rain that falls into a shallow layer of subfreezing air at the ground (usually only several hundred feet deep) and freezes upon impact to form a coating of glaze on exposed objects.

Rain:Liquid precipitation in the form of water drops with diameters greater than 0.020 inch. Drizzle, the only other form of liquid precipitation, consists of droplets 0.020 inch in diameter or smaller.

Sleet: Precipitation in the form of small ice pellets. Sleet forms when raindrops (or largely melted snowflakes), originating in warmer air aloft, fall through a layer of subfreezing air at ground level and then freeze on their way down. Sleet is often referred to as ice pellets in weather observations.

February 4, 2008

Understanding the Weather: Feb. 4, 2008

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Chicago's snowiest Februarys
1885-2007 snowfall data

27.8" 1896
26.2" 1994
23.7" 1980
22.6" 1900
22.5" 1967

February 2, 2008

Understanding the Weather: Feb. 2, 2008

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Chicago's biggest February snowstorms
(1885-2007)

13.4" Feb 6-7, 1895
12.8" Feb 18-19, 1908
12.7" Feb 6-7, 1933
12.5" Feb 3-4, 1896
12.2" Feb 3-4, 1901
12.0" Feb 12-13, 1896

January 31, 2008

Understanding the Weather: January 31,2008

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Chicago's largest day-to-next temperature changes
In the period Nov. 1, 1870, through Jan. 30, 2008

temperature rises
58º from 0º to 58º February 13-14, 1887
58º from 15º to 73º March 10-11, 1972
57º from 24º to 81º March 31-April 1, 2003

temperature falls
61º from 74º to 13º November 11-12, 1911
58º from 62º to 4º February 8-9, 1900
58º from 49º to -9º December 13-14, 1901

January 28, 2008

Understanding the Weather: Jan. 28,2008

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Arctic air: A type of air mass whose characteristics are developed in the cold season over ice- and snow-covered areas of the far north. It has low temperatures, low moisture content, and is very stable. Air masses of arctic origin cover Chicago about six percent of the time.

Arctic outbreak: The rapid movement of a mass of air originating above the Arctic Circle southward to the Gulf of Mexico, or farther. Arctic outbreaks bring Chicago its lowest autumn and winter temperatures; also called "polar outbreak."

Cold wave: In popular usage, a period of very cold weather. Meteorologically, a rapid fall in temperature within 24 hours to temperatures requiring substantially increased protection to agriculture, industry, commerce and social activities.

Norther: In popular usage in the southern United States, especially Texas, a strong cold wind from the northwest, north or northeast. It is the cold outbreak associated with the southward movement of a frigid air mass.

Blue norther: In popular usage in the Southern Great Plains, a blast of bitterly cold arctic air that surges south across Texas during the winter, bringing strong north winds and a sudden, sharp temperature drop.

January 25, 2008

Understanding the Weather: Jan. 26, 2008

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Chicago snow facts
(based on 123 years of snow statistics beginning with the winter of 1884-85)

8.2 inches

On average, that is the largest snowstorm that Chicago can expect in any given winter season.

In Chicago, the winter's biggest snowstorm has ranged from a puny 2.4 inches during the 1921-22 snow season to 23.0 inches in 1966-67.

January 24, 2008

Understanding the Weather: Jan 24, 2008

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Cryosphere: The portions of the Earth (in the atmosphere, at the surface, in the ground) in which water is in solid form. It includes snow and ice crystals in the air, snow cover and ice caps, floating ice (on rivers, lakes, oceans), glaciers, permafrost, etc. The word is derived from the Greek "kyros," meaning frost or icy cold.

Intergelisol: A sub-surface layer of frozen ground that might persist for a few years but is not permanently frozen ground and is not considered to be permafrost (soil and rock whose temperature is permanently at or below 32 degrees).

Mollisol: In regions of permanently frozen underlying soil, mollisol is the surface layer that freezes in the winter and thaws in the summer. It varies in thickness from a few inches to several feet.

Pereletok: A sub-surface layer of frozen ground that might persist for a few years, but is not permanently frozen and is not considered to be permafrost. The term is Russian, meaning "survives over the summer."

Permafrost: Permanently frozen ground; it underlies about 85 percent of the state of Alaska, and in northern Alaska it reaches its greatest thickness, about 2,000 feet.

Subgelisol: Unfrozen ground beneath permafrost.

Talik: Permanently unfrozen ground in regions of permafrost.

January 21, 2008

Understanding the Weather: Jan. 21, 2008

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Icebox of the nation

Communities claiming to be the “nation’s icebox” include Pellston, Mich., International Falls, Minn., Fraser, Colo., Truckee, Calif., Stanley, Idaho, and West Yellowstone, Mont. Here are their average annual temperatures. You be the judge.

34.8º Fraser, Colorado
35.4º Stanley, Idaho
36.5º International Falls, Minnesota
40.2º West Yellowstone, Montana
42.7º Pellston, Michigan
44.4º Truckee, California

January 20, 2008

Understanding the Weather: Jan. 20, 2008

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-20ºF

At Chicago, temperature readings that cold (or colder) are exceedingly rare occurrences. So rare, in fact, that they have appeared only 15 times since the inception of Chicago's official temperature records on November 1, 1870.

If you experienced any of them, chances are you have a vivid memory of the event.

Here they are, listed in chronological order:

1 -21º Sunday, Dec. 22, 1872
2 -23º Tuesday, Dec. 24, 1872
3 -20º Saturday, Jan. 9, 1875
4 -20º Monday, Jan. 25, 1897
5 -21º Thursday, Feb. 9, 1899
6 -26º Sunday, Jan. 10, 1982
7 -25º Saturday, Jan. 16, 1982
8 -23º Sunday, Jan. 17, 1982
9 -21º Friday, Dec, 23, 1983
10 -25º Saturday, Dec. 24, 1983
11 -20º Friday, Jan. 20, 1984
12 -22º Saturday, Jan 21, 1984
13 -23º Saturday, Jan. 19, 1985
14 -27º Sunday, Jan. 20, 1985
15 -21º Tuesday, Jan. 18, 1994

January 19, 2008

Understanding the Weather: Jan. 19, 2008

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Wind chill temperature: The temperature of still air that would remove heat from an exposed human body as quickly as it is being removed by the existing combination of actual air temperature and wind speed. Humidity and evaporative cooling are not taken into consideration.

Apparent temperature: The heat index; using air temperature and relative humidity, how hot it feels to an "average" person (147 pounds) wearing light clothing and walking 3.1 m.p.h. in a wind that is blowing 5 m.p.h.

Temperature: A measure of the internal energy that a substance contains. The degree of hotness or coldness of a substance, or of the environment. Air temperature is the most frequently measured atmospheric variable.