Ch. 3, section 1 Seasons and Weather

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Seasons and Weather Chapter 3, Section 1

Transcript of Ch. 3, section 1 Seasons and Weather

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Seasons and Weather

Chapter 3, Section 1

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Seasons

Earth is tilted at a 23.5˚ anglecauses different areas to get direct sun rays for different

amounts of time creating seasons

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Seasons

Tropic of Cancer and Tropic of Capricorn are the farthest points north and south where the sun shines directly overhead at noon – solsticebeginning of winter or

summer

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Summer Solstice

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Winter Solstice

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Equinox

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Seasons

Equinox – twice a year when the days and nights are the same all over the worldbeginning of spring and fall

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Weather - immediate condition of the atmosphere at a specific location and time

climate – general weather conditions over a long period of time

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What causes weather?water vapor causes precipitationcloud cover holds water vapor

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What causes weather?

landforms and bodies of water water heats and cools slowly

land heats and cools quickly

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What causes weather?

elevation higher elevation = thinner air (doesn’t hold moisture)

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What causes weather?

air movement wind moves air and moisture causes rapid weather changes

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Precipitation

Warm air rises air cools clouds form water vapor builds up pressure releases and it rains

3 types

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Convectional

Hot, moist climateHeat air in the morning, clouds form by

afternoon and rain falls

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Orographic - mountains

Windward side (wet side) of mountain blocks air and forces it up

Leeward side (dry side) has a rain shadow (very little precipitation)

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Frontal

Mid-latitudeBoundary between 2 air masses with

different temperaturesCold air pushes warm air up =

precipitation

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Weather Extremes

blizzards – heavy snowstorm with winds > 35 mph

drought – long period of time with little or no rain

Floods – water spreads over usually dry land

Flood plain – when water spills out of a river into surrounding area

Hurricanes

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• Hurricane winds also cause storm surges (water flooding in from the ocean) 15 feet or more.

• This is what did the most damage to Galveston in the 1900 hurricane. The highest point on the island was only 8.5 feet. The storm surge was over 15 feet.

• 6,000 to 12,000 people died and the clean up was horiffic.

• To prevent such damage again, a 17 foot wall was built and the entire city was raised 17 feet

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Damage to Galveston after the 1900 hurricane

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Galveston Seawall

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Raising Galveston

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• They moved about 440 million cubic feet of sand into the city.

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• Everything was raised between a few inches to 17 feet, including the 6 million pound St. Patrick’s Church.

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Galveston was known as the New York of the South. It was the largest, most developed, and most modern city in Texas. Houston was a backwater, a “country-bumpkin” town compared to Galveston. After the 1900 hurricane, though, development shifted to Houston and Galveston was forever left behind.

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Hurricane Rita

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IKE

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Blizzards

• Massive snowstorm with high winds

Drought

• Long period with little or no rain

• Damages crops, plants, and wildlife

• Can also cause massive wind erosion, as in the Dust Bowl of the early 1930’s.

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Blizzards

• Massive snowstorm with high winds

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In South Dakota

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Floods

• Lots of rain or runoff causes rivers and streams to overflow their banks

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