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Aim: How does atmospheric pressure generate winds?

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Presentation on theme: "Aim: How does atmospheric pressure generate winds?"— Presentation transcript:

1 Aim: How does atmospheric pressure generate winds?

2 How are the winds moving in this hurricane?

3 How can we describe this map?
Isobars – lines which connect points of equal pressure Pressure gradient – rate of change in pressure between two locations Steep pressure gradient: Isobars close together – strong (high) wind speeds Gentle pressure gradient: Isobars far apart – gentle (low) wind speeds

4 How does wind move? Winds a move from high pressure areas to low pressure areas, resulting from uneven heating of Earth's atmosphere How do we measure wind speed and direction? Anemometer – instrument used to measure wind speed Wind vane – instrument used to measure wind direction

5 Cyclones (Low Pressure) Anticyclones (High Pressure) Warm & moist air
Precipitation Cool, dry air Bad Weather Good Weather Condensation occurs Air contracts – more dense (sinks) A Air cools & expands B Warm, wet air rises – less dense Air warms up due to compression L Winds flow High to Low H Cyclones (Low Pressure) Anticyclones (High Pressure) Warm & moist air Cool & dry air Lowest pressure in the center Highest pressure in the center Winds move to center (converge) Winds move out of center (diverge) Winds rotate counter clockwise 960 940 920 L 960 940 920 L Winds rotate clockwise 1003 1004 1005 H 1003 1004 1005 H Pressure increases outwards Pressure decreases outwards 960 1003 940 1004 920 1005 Lo Co LICC L H Hi Di HOC

6 Water: cooler, heats up slower, high specific heat
High Pressure Low Pressure Low Pressure High Pressure Cold Temp Warm Temp Warm Temp Cold Temp Sea Breeze – wind flow from high to low Land Breeze Land: warmer, heats up faster, low specific heat Water: cooler, heats up slower, high specific heat Water: warmer, cools down slower, high specific heat Land: cooler, cools down faster, low specific heat Sea Breeze – winds flow from water to land Land Breeze – winds flow from land to water

7 Mountain Windward Side “Low Pressure” Leeward Side “High Pressure”
Adiabatic Cooling Adiabatic Warming Windward Side “Low Pressure” Leeward Side “High Pressure” Air cools to dewpoint temp, condensation occurs Cool, dry air Sinks – more dense Cools & expands Air warms due to compression (molecules come closer together) Warm, wet air rises – less dense Mountain Prevailing Winds Rainforest Cool & Wet Desert Warm & Dry

8 Answer the questions on the worksheet
Summary Activity Answer the questions on the worksheet The diagram below shows the isolines of air pressure around a low-pressure center. On which side of the low-pressure center will the wind speed be greatest? East

9 Extra Questions

10 1003 1004 1005 H 960 940 920 L

11 Winds move to center (converge) Winds rotate counter clockwise
Low Pressure High Pressure A B L H (Low Pressure) (High Pressure) Warm & moist air Cool & dry air Lowest pressure in the pressure in the center Winds move to center (converge) Winds move out of center (diverge) Winds rotate counter clockwise Winds rotate clockwise Pressure increases outwards Pressure decreases outwards L 960 940 920 L H


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