what is weather? weather patterns weather forecasts

Download What is Weather? Weather Patterns Weather Forecasts

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What is Weather? Weather Patterns Weather Forecasts Slide 2 Weather : state of the atmosphere at a specific time and place Weather describes conditions such as air pressure, wind, temperature and amount of moisture in air Sun provides almost all of earths energy It encourages evaporation, which condenses and water returns to earths surface The land absorbs the heat and warms the atmosphere and causes uneven heating of atmosphere Air and water currents are caused by suns uneven heating Slide 3 Temperature is a measurement of the motion of molecules The more movement, the greater the temperature Less movement of molecules, the cooler the temperature Slide 4 Air moving in a specific direction is called wind Air near the surface is warmed by conduction Air expands, becomes less dense, rises (warm rising air forms low pressure at surface) Cool dense air tends to sink that yields to high pressure areas Wind results because air moves from areas of high to low pressure Slide 5 Wind direction is measured by a wind vane (points in the direction from which wind is blowing) Wind is measured by an anemometers which has cups that spin with wind strength Slide 6 When water evaporates into the atmosphere it fits into spaces The amount of water vapor present in an air mass is called humidity Warmer air can hold more water vapor Cooler air holds less water If temperature is cool enough water vapor condenses and the air mass is considered saturated Slide 7 Relative humidity is a measure of the amount of water vapor present in the air compared to amount needed for saturation at a specific temperature Relative humidity is dependent on the specific temperature and changes as temperature changes (warmer air holds more water than cooler air) If a cubic meter of air at 25C is saturated with 22 g of H 2 O it is said to have a RH of 100% If it has 11 g of H 2 0 it has RH of 50% Slide 8 When temperature drops, less water vapor can be held and it condenses to a liquid or forms ice (depending of the temperature) The temperature at which condensation occurs is called Dew Point Slide 9 Warm air rises As air rises it cools Cooler air doesnt hold as much water and if it cools to saturation point, its dew point is met Water droplets form around nuclei of dust, smoke, smog to form clouds after saturation point is met Slide 10 Classified by shape and height Shape and height of clouds vary with temperature, pressure, and amount of water vapor present Slide 11 3 Main types Stratus (form layers or smooth even sheets) Found at lower altitudes and may be associated with fair weather or rain or snow Fog is low stratus clouds formed by saturation near ground level Slide 12 Stratus Clouds : low and flat Slide 13 Cumulus clouds: masses of puffy white clouds often with flat bases Sometimes they tower to great heights and can be associated with fair weather or thunderstorms Slide 14 http://images.search.yahoo.com/search/ima ges;_ylt=A2KJkIbcDaRP5HIAdx2jzbkF?fr2=xpl &p=cumulus+clouds&fr=slv1-mdp&vm=r http://images.search.yahoo.com/search/ima ges;_ylt=A2KJkIbcDaRP5HIAdx2jzbkF?fr2=xpl &p=cumulus+clouds&fr=slv1-mdp&vm=r Slide 15 Cirrus clouds: appears fibrous curly, wispy They are high, thin, white feathery made of ice crystals Associated with fair weather, or can indicate approaching storms Slide 16 http://images.search.yahoo.com/search/ima ges;_ylt=A2KJke4JFqRPyHUAIQWjzbkF?fr2=xp l&p=cirrus+clouds&fr=slv1-mdp&vm=r http://images.search.yahoo.com/search/ima ges;_ylt=A2KJke4JFqRPyHUAIQWjzbkF?fr2=xp l&p=cirrus+clouds&fr=slv1-mdp&vm=r Slide 17 Prefixes help describes the height of clouds Cirro (high clouds) Alto (middle clouds) Strato (low level clouds) Some combine the altitude with stratus or cumulus Cirrostratus (high clouds-fair weather or warning of approaching storm) Altostratus: not thick, middle layers, sunlight filters through Slide 18 Nimbus (dark rain cloud) refers to clouds that produce rain or snow Because they are thick, you cant see through them Cumulus clouds grows into thunderstorms called cumulonimbus (12 miles up) Nimbostratus clouds are layered clouds that can bring long steady rain or snowfall Slide 19 Slide 20 Slide 21 http://images.search.yahoo.com/search/ima ges;_ylt=A2KJkPkgD6RPrFQAcAmjzbkF?p=ni mbostratus%20clouds&ei=utf- 8&n=30&x=wrt&tab=organic&fr2=sg- gac&sado=1&vm=r http://images.search.yahoo.com/search/ima ges;_ylt=A2KJkPkgD6RPrFQAcAmjzbkF?p=ni mbostratus%20clouds&ei=utf- 8&n=30&x=wrt&tab=organic&fr2=sg- gac&sado=1&vm=r Slide 22 Water falling from clouds is known as precipitation Water grows around nuclei (dust, smoke) and grow larger until they fall to ground Raindrop size depends on strength of updrafts in cloud (strong updrafts let condensed water move up and down, growing in size) If the temperature is warm as droplet falls it can evaporate before reaching surface Slide 23 Air temperature determines whether water forms rain, snow, sleet, or hail Above freezing falls as rain Snow forms when temperatures is so cold that water vapor changes directly to a solid Sleet forms when raindrops pass through layers of freezing air near surface forming ice pellets Slide 24 Hail is precipitation in the form of lumps of ice Forms in cumulonimbus clouds when thunderstorms develop Hailstones grow as they are tossed up and down in cloud Can grow from 2.5 cm (1inch) to softball size Slide 25 Relative humidity helps determine whether you will have a dry or wet day The temperature of atmosphere determines the form of precipitation Winds are dependent on rising air Slide 26 Air Mass: large bodies of air that have properties similar to the part of the earths surface over which they develop Continental polar: develops over continent (dry) and cold Continental tropics: develops over continent (dry) and warm Maritime polar: develop over body of water (moisture) and is cold Maritime tropics: develop over water and warm Slide 27 Slide 28 Winds blow from high pressure to low pressure Pressure is measured by amount of air above the surface As winds blow into low pressure systems, the rotation of earth causes low pressure systems to move counter-clockwise called cyclone Low pressure are areas of rising air (temperature decreases, clouds form, precipitation probable) Slide 29 Winds that blow from High pressure spiral clockwise in northern hemisphere (anticyclone) High pressure is associated with fair weather Barometers measure the pressure above the surface Variations of pressure in atmosphere affects weather Sinking air in high pressure systems indicates warming air mass, less clouds (or no) usually is fair weather Slide 30 Slide 31 Boundary between two air masses of different density, moisture, or temperature is called a front Cloudiness, precipitation and storms sometimes occur Slide 32 Cold front is shown on map with a blue line with triangles pointing in direction of air mass movement ( when colder air advances toward warm air) Cold air wedges and lifts warm air upward Warm air cools, clouds form (if enough moisture) Thunderstorms form when temperature differences are large Slide 33 Warm front forms when warm air advances over heavier colder air It is written with red lines and semi-circles pointing in the direction of the warm air advances Slide 34 This involves 3 air masses of different temperature Cold air moves toward cool air with warm air between the two Colder air is forced up, closing off the warm air from the surface Shown on maps with purple lines with triangles and semicircles Slide 35 When boundary between air mass stop advancing Remain in same place for several days, producing light wind and precipitation Shown as alternating warm and cold front symbols Slide 36 Slide 37 Slide 38 Thunderstorms : occurs when warm moist air rises along fronts Cumulonimbus clouds form that can reach heights of 12 miles up In cloud smaller droplets of water collide to form bigger ones As droplets fall, the air is cooler, and brings about updrafts of warmer air causing strong winds Hail forms in clouds if temperature is below freezing in the clouds and droplets freeze in up and down drafts Slide 39 Slide 40 Slide 41 Flash flooding occurs when streams cant contain all the water Strong winds originating from the thunderstorm causes damage Hail damages property Destroy crops Slide 42 Lightning: warm air is lifted faster in clouds when clouds form as cooler air sinks Movement of air can cause different parts of the cloud to be oppositely charged Currents then flow in opposite direction causing lightning Lightning can occur cloud to cloud, cloud to ground and within a cloud Slide 43 Lightning can reach temperatures of 30,000 C (suns photosphere is 6000C) This extreme heat causes air around the lightning to expand rapidly Then it cools quickly and contracts That rapid movement of the molecules forms sound waves heard as thunder Slide 44 Tornados are violent rotating columns of air in contact with the ground In thunderstorms, wind at different heights blow at different speeds These differences are called wind shear and rotates the column parallel to ground It can create a funnel cloud as it rotates upward If it touches the ground it is called a tornado Slide 45 Hurricanes are large swirling low pressure system that originates over warm oceans It moves warm air away from the ocean to the atmosphere as wind Typhoons and cyclones are another name In the Atlantic Ocean hurricanes develop near Africa and winds direct them to U.S. Gain strength as move over warm oceans When hurricanes reach land they cause destruction and damage, tornados spin off but land cuts off their energy source, so they are de-energized and loose power Slide 46 Slide 47 Slide 48 Blizzards in the northwest are common Temperatures must be low as well as visibility (400m) caused by blowing winds (56 mph) Slide 49 Mete


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