the wonderful world of weather. factors affecting weather

The Wonderful World of Weather

Factors Affecting Weather

• As the earth revolves around the sun it is tilted at 23.5 degrees

• Because of the earth’s revolution and tilt direct sunlight hits the earth differently at different parts causing changing seasons on the earth

Earths Tilt

Mark points farthest north and south that the sun’s rays shine directly overhead at noon

• The day on which this occurs is called a solstice

The Tropic of Cancer and Tropic of Capricorn

• In the Northern Hemisphere the summer solstice begins summer, the longest day of the year. The winter solstice begins winter the shortest day of the year

Winter Solstice in Northern Hemisphere Summer Solstice in Northern Hemisphere

• This is another sign of changing seasons

• Occurs 2 times a year when the days and nights all over the world are equal in length.

• Marks the beginning of Spring and Autumn

Equinox

Types of Precipitation

Convectional: Typical of hot climate (Tropical)

• Occurs after morning sunshine heats warm moist air.

• Clouds form in the afternoon and rain falls

Clouds forming over the Florida peninsula.What time of day do you think this picture was taken?

Orographic: Associated with mountain areas• Mountains block the passage of air and cause it to rise

• Storms drop more rain on the windward side and create a rain shadow on the leeward side because it gets little rain from the descending dry air

Moist air rises and cools on windward side of mountains

Condensation occurs and precipitation results

Drier air descends down the mountains and warms

Leeward side of mountain range has rain shadow desertMT

RANGE

WINDWARD SIDE

LEEWARD SIDE

In which part of the United States will you find orographic precipitation?Where is the rain shadow?

Mount Waialeale on the island of Kauai in Hawaii has the greatest annual average of precipitation (486” per year or 40. feet).The backside (leeward) side of the mountain gets only 20” of rainfall per year.

Cherrapunjee (on the south side ofThe Himalayas) holds the all-time record for precipitation in one year.

Frontal: Mid-latitude frontal storms

• Cold, dense air pushes warm, light air upward causing precipitation to form

Landforms

• Landmasses heat and cool relatively quickly; there are wider temperature ranges in the interior of large landmasses.

Large Bodies of Water

• Water heats and cools more slowly than adjacent landmasses, so it moderates temperatures there. (It doesn’t get as cold or as hot.)

Cold and Warm Ocean Currents

Elevation• As elevation increases above sea level, temperature

decreases. (Compare the current temperature in Mexico City to that of Austin?)

• The air cools and becomes thinner and loses its ability to hold moisture.

Air Movement• winds move air and moisture• As a result weather can change very rapidly

Prevailing Winds

Pressure Systems

Wind will flow from high pressure zones towards low pressure zones.Low pressure zones are associated with rain as warm air rises and releases moisture.

• http://ww2010.atmos.uiuc.edu/(Gh)/guides/mtr/fw/gifs/coriolis.mov