Mindmap
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Inhalt der Mindmap
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CLOUDS
- Stratus
- Nimbostratus
- Large dark sheets of clouds. Indicate rain or snow.
- low altitude
- indicates chance of light mist or drizzle
- Nimbostratus
- Cumulus
- Cumulonimbus
- large and darker cumulus clouds
- dense, towering vertical cloud
- thick and puffy on top, flat on bottom
- high altitude
- Cumulonimbus
- Cirrus
- ends curl and feathery look
- high altitude
- Stratus
HOW CLOUDS FORM
- 1. Evaporation turns water into water vapor
- 2. Temperature gets cooler and reaches dew point
- 3. Water vapor turns back into liquid due to condensation and sticks to dust particles
- 2. Temperature gets cooler and reaches dew point
- 1. Evaporation turns water into water vapor
VOCABULARY
- Water vapor - water in gaseous form
- Dewpoint - the temperature at which water vapor condenses
- Global winds - winds that move over a long distance
- Climate - average weather over a long period of time
- Humidity - amount of water vapor in the air
- Atmosphere - the mixture of gas that surrounds a planet
- Air temperature - the measure of the force pushing on the surface of the Earth
- Precipitation - any form of water that falls on Earth
- Air temperature - the measure of the force pushing on the surface of the Earth
- Atmosphere - the mixture of gas that surrounds a planet
- Humidity - amount of water vapor in the air
- Climate - average weather over a long period of time
- Global winds - winds that move over a long distance
- Dewpoint - the temperature at which water vapor condenses
- Water vapor - water in gaseous form
LAYERS OF THE ATMOSPHERE
- Exosphere
- Thermosphere
- Mesosphere
- Stratosphere
- Troposphere
- lowest layer with life forms
- 9 miles - distance to earth
- 15 C to -52 C
- weather, gases, clouds, birds, airplane, and kites/balloons are found here
- 15 C to -52 C
- 9 miles - distance to earth
- lowest layer with life forms
- 31 miles - distance to earth
- contains the ozone layer which protects everything of earth from UV rays
- -52 C to -3 C
- commercial jets and Weather balloons are found here
- OZONE LAYER
- the thickness of the ozone layer can change in between seasons
- absorbs most of the solar radiation coming from the sun
- Protects everything living on Earth from the sun's UV rays
- contains high concentration of ozone
- the ozone layer is declining due to pollution/chemicals created by humans
- contains high concentration of ozone
- Protects everything living on Earth from the sun's UV rays
- OZONE LAYER
- commercial jets and Weather balloons are found here
- -52 C to -3 C
- contains the ozone layer which protects everything of earth from UV rays
- Troposphere
- protects earth from meteors and space "junk"
- Ice crystals and meteors are found here
- 53 miles - distance to earth
- -3 C to - 90 C
- 53 miles - distance to earth
- Ice crystals and meteors are found here
- Stratosphere
- -90 C to 1800 C
- Northern lights and space shuttle are found here
- 310 to 621 miles - distance to earth
- Northern lights and space shuttle are found here
- Mesosphere
- 1800 C
- Satellites are found here
- Outermost limits of earth and very thin air
- 620 miles - distance to earth
- Outermost limits of earth and very thin air
- Satellites are found here
- Thermosphere
- Earth's atmosphere is always moving due to the sun's uneven heating upon earth
- Exosphere
WIND
- Cold air is dense and sinks
- warm air is less dense and rises
- The motion of warm air rising and cool air sinking happens in a circular path - a.k.a convection current
- warm air is less dense and rises
- wind is formed by the heat of the sun and the rotation of the earth
- GLOBAL WINDS
- winds that move over long distances between the equator and poles
- warm air rises at the equator
- cold air sinks at the poles
- the earth tilts as it's rotating = global winds don't move in a straight path
- these winds circle the globe from the right of the Northern Hemisphere to the left of the Southern Hemisphere
- the earth tilts as it's rotating = global winds don't move in a straight path
- cold air sinks at the poles
- warm air rises at the equator
- 3 Types of Global Wind Systems
- Trade winds
- winds that blow from a 30-degree latitude to the equator and curve to the west as moving towards the equator
- Westerlies
- winds that occur between a 30-degree and 60-degree latitude towards the poles from west to east. They typically bring moist air with them.
- Easterlies
- Polar easterly winds form when cold sinking moves between the poles. 60-degree latitude
- Trade winds
- winds that move over long distances between the equator and poles
- Cold air is dense and sinks
Informationen
- Beschreibung
- 10th grade Science Mindmap am --, erstellt von Mehal Bhattacharya am 19/11/2018.
- Erstellt von
- Mehal Bhattacharya · Nov 2018
- Aktualisiert
- 20 Nov 2018
- Aufrufe
- 0
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