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Mr. Fetch’s Earth Science Classroom. Temperature – a measurement of heat Temperature is a factor of particle motion. Faster moving particles create more.

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Presentation on theme: "Mr. Fetch’s Earth Science Classroom. Temperature – a measurement of heat Temperature is a factor of particle motion. Faster moving particles create more."— Presentation transcript:

1 Mr. Fetch’s Earth Science Classroom

2 Temperature – a measurement of heat Temperature is a factor of particle motion. Faster moving particles create more heat Temperature is measured with a thermometer

3 Mr. Fetch’s Earth Science Classroom Wind Wind is moving air It is caused by differences in air pressure within the atmosphere.air pressureatmosphere Air under high pressure moves toward areas of low pressure

4 Mr. Fetch’s Earth Science Classroom Barometric Pressure Atmospheric/air pressure is measured with a barometer in units of inches of mercury or millibars Barometric pressure is the force exerted on objects by the weight of the atmosphere above them.

5 Mr. Fetch’s Earth Science Classroom Precipitation: -Precipitation is rain, sleet or snow, precipitation is any product of the condensation of atmospheric water vapour that falls under gravity

6 Relative Humidity Relative humidity is a measure of the amount of water vapor in the air compared to the maximum amount of water vapor the air can hold at that temperature. A psychrometer is one instrument that measures relative humidity.

7 Dew Point and Humidex The dew point is the temperature which water vapor in air will condense into liquid water. Condensed water is called dew when it forms on a solid surface (like grass) or a cloud when it forms in the sky. The humidex (short for "humidity index") is a number used to describe how hot the weather feels to the average person. The humidex is a unit-less number based on the dew point, and is equivalent to the dry temperature in degrees Celsius.

8 The Coriolis Effect Caused by the Earth’s rotation Results in the curving of moving objects, including air It is one thing that causes wind and the direction of prevailing winds that exist in each major latitude belt

9 Weather Fronts The boundary between 2 air masses with different temperatures Brings about a change in weather

10 Prevailing Wind The direction the wind blows most of the time in a certain location

11 Is - the branch of science dealing with weather forecasting. Atmospheric conditions that are typically measured to provide information for weather forecasts and to study the weather and climate include:  temperature  barometric pressure  humidity  wind speed & direction  precipitation

12 Mr. Fetch’s Earth Science Classroom Barometer Device used for measuring Atmospheric/air pressure in units of inches of mercury or millibars

13 Mr. Fetch’s Earth Science Classroom

14 1. Air Pressure is always changing and depends on factors such as: Temperature/Time of day - hotter air has higher pressure Altitude – higher up = lower pressure Humidity – higher = lower pressure Migrating weather systems – Highs and Lows

15 2.Represented on a weather map by isobars with an “H” (High Pressure) in the central most isobar isobars with an “L” (Low Pressure) in the central most isobar

16 Highs and Lows on Weather Maps

17 3.Jet Streams Narrow currents of fast moving air flowing in the upper levels of the atmosphere Flow between cold and warm air masses Usually move weather systems from place to place – always WEST to EAST

18 4. Humidex The humidex (short for "humidity index") is a number used to describe how hot the weather feels to the average person. The humidex is a unit-less number based on the dew point, and is equivalent to the dry temperature in degrees Celsius.

19 5. Warm Front Along a front the warm air mass will always be forced up as opposed to the cold air mass. Warm air is less dense and therefore will lift more easily than cold air which is more dense.

20 Cold Front Passes quickly through an area…sometimes as fast as 100 km/hr

21 Occluded Front

22 The Coriolis Effect Caused by the Earth’s rotation Results in the curving of moving objects, including air It is one thing that causes wind and the direction of prevailing winds that exist in each major latitude belt

23 Mr. Fetch’s Earth Science Classroom

24 Wind, clouds, and precipitation are all the result of the atmosphere responding to uneven heating of the Earth by the Sun. The uneven heating causes temperature differences, which in turn causes wind, which then moves the heat to a new place.

25 m What causes weather? Caused by the transfer of energy between these 3 things: - The Sun, Earth’s surface, and the Atmosphere. Hot air rises and cools The sun warms earth’s surface - increasing its temperature. Water vapor condenses to form clouds & precipitation The sun’s energy is used to evaporate water and put moisture into the air. Unequal heating and differences in air pressure cause wind

26 2. Cold FrontsWarm Fronts CONTRASTCONTRAST Created when a cooler air mass overtakes a warmer air mass. Warm air rises b/c it is pushed up by the cool air and b/c it is less dense. Steeply sloping curved line front. Heavy rain and wind. Passes through quickly. Cool, dry, and clear skies after Mainly cumulus type clouds Created when warmer air mass overtakes a cooler air mass. Warm air rises just b/c it is less dense. Gentle sloping straight lined front. Light rain and wind. Passes through slowly. Warm, humid, and cloudy after. Mainly stratus type clouds.

27 3. Weather from Cold Front As Approaching /Front line Heavy rain and wind. Passes through Quickly After Cool, dry, and clear skies after front passes through.

28 Warm Front Created when a warmer air mass slowly overtakes a cooler air mass (Both Traveling in same Direction) When the faster moving air meets up with the slower moving cooler air, the warmer (less dense) air rises slowly and gently above the cooler air mass. Weather changes slowly. Creates a gently sloping, straight lined “Front”. As the warm air rises, it cools, and causes water vapour to condense.

29 Warm Front Passes slowly through an area – a couple of days Add

30 Cold Front Created when a fast moving cool air mass rapidly overtakes slower warmer air mass. When the faster moving cooler air meets up with the slower moving warm air, the cooler air forces the warm air to rise more quickly than it otherwise would rise. Weather changes rapidly. Creates a steeply sloping, curved “Front”. Almost verticle. As the warm air rises, it cools, and causes water vapour to condense.

31 Cold Front Passes quickly through an area…sometimes as fast as 100 km/hr

32 Stationary Front Weather is similar to a warm front but transition is slower and gentler yet. When the two masses of air meet, neither has enough force to move the other. The two air masses face each other in a “stand off”- they both stop moving. Temperature and wind direction are opposite on either side of the front line. At the junction of the cold and warm air masses, clouds will form and precipitation will occur. Can remain stalled over an area for days.

33 Stationary Front Can remain stalled over an area for days

34 Occluded Front A faster moving cold air mass overtakes a slower moving warm air mass. A warm air mass gets caught in between two cold air masses. The warm air forced up, causing clouds to form. The clouds may result in rain or snow.

35 Occluded Front

36 What Causes Wind (Short Answer) Wind is caused by air flowing from high pressure to low pressure. The Earth's rotation prevents that flow from being direct, but deflects it side to side(right in the Northern Hemisphere and left in the Southern), so wind flows around the high and low pressure areas.

37 Why do High Pressure Systems cause weather to stay longer? (Short Answer Question) Because High Pressure systems are large, usually the size of an entire air mass, therefore they take a longer time to move out of an area.

38 Mr. Fetch’s Earth Science Classroom

39 Precipitation: Change of State MELTING Uses Heat FREEZING Gives off Heat Sublimation Uses Heat Deposition Gives off Heat Uses Heat EVAPORATION CONDENSATION Freezing/Melting point of water/ice is 0 0 C + Add energy - Subtract energy

40 Temperature Profile of a Frontal System


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