F. Adiabatic Changes and Cloud Formation

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Presentation transcript:

F. Adiabatic Changes and Cloud Formation Temperature changes without __________ of heat with the surroundings. Temperature rises without the addition of heat. Temperature falls without the loss of heat. exchange

Adiabatic Cooling Expansion of air: Causes gas molecules to move _______________. Air temperature ______________. Caused by air ___________ (as it rises) and the ___________ air pressure around the parcel of air. less rapidly decreases expanding decreasing

Adiabatic Heating Compression of air: Gas molecules more ___________________. Air temperature ______________. Caused by air being ___________ (as it sinks) by the ___________ air pressure around the parcel of air. more rapidly increases compressed higher

Lapse Rate (not in Notes)

Lifting Condensation Level Altitude at which rising air has cooled to its __________temperature. The lifting condensation level will be the altitude of the ____________. dew point cloud base

Finding the Lifting Condensation Level

Finding the Lifting Condensation Level

Finding the Lifting Condensation Level Dry Bulb = 20o C Dew Point = 4o C

Finding the Lifting Condensation Level Dry Bulb = 20o C Dew Point = 18o C Cloud Base 0.25 km

Requirements for Cloud Formation ________ air b. _____________ (hydroscopic) Nuclei Salt particles from ocean spray, volcanic dust, pollen, smoke, etc. c. _________temperatures: Most often caused by unstable air. So, what is the difference between unstable air and stable air? Humid Condensation Cooling

(1) Unstable Air rise Air that has a tendency to ________. The lowermost portion of the atmosphere is warmed to a higher temperature than the air aloft. rise Air that has a tendency to ________. It will rise until it reaches an altitude where its temperature is equal to that of the surrounding air. As it rises it will cool adiabatically.

(2) Stable Air Tends to _________in its original position or if forced to rise will tend to sink. It’s cooler (and denser) than the surrounding air remain

(3) Causes of Lifting Localized Convective Lifting __________heating of Earth’s surface causes pockets of air to become warmer than its surroundings. The parcels rise, causing __________. Unequal thermals

(b) Convergence together Air in the lower troposphere flows __________. Lifting results as air piles up.

(c) Orographic Lifting Windward Leeward Cool and Wet Warm and Dry Mountain barriers force air to rise on the ___________side. Air becomes__________. Air descends on the ________side and heats by compression (dry adiabatic rate) ________________deserts result on the leeward side. windward unstable leeward Rainshadow

(d) Frontal Wedging ___________________produced by collision of warm and cold air masses. Warm air forced _______cooler air, forming middle-latitude cyclones (wave cyclones). Boundaries (fronts) over

Warm Air is Forced to Rise Along a Frontal Boundary The parcel of air is cooler than the surrounding air up to nearly 3,000 m and has a tendency to sink (stability) Above 3,000 m the parcel is warmer than the surrounding air and will rise. (It’s unstable.) The result can be towering cumulus clouds.

Classification of Clouds Classification by Cloud Form Cirrus High altitude clouds made primarily of ice crystals. Are thin and white due to small amount of water vapor at high altitudes. Cumulus Individual masses and often form on clear days. Often develop into vertical domes or towers. Stratus A uniform layer that frequently covers much of the sky. Layered clouds due to horizontal air flow (4) Nimbo or Nimbus – Rain or Snow descends.

6. Classification by Height High Clouds: Above 6000 meters (20,000 ft): Clouds in this “family” are thin, white, and composed primarily of ice crystals due to small amounts of water vapor and low temperatures Middle Clouds: Altitude range of 2000 to 6000 meters (6500 to 20,000 ft) Low Clouds: Base below 2000 m (6500 ft) Clouds of Vertical Development Do not fit into any of the three height families of clouds Bases are low and tops extend to the middle or high altitude range and are associated with unstable air.

Cloud Type (name?)

Cloud Type (name?)

Cloud Type (name?)

Cloud Type (name?)

Fog A cloud with its base at or very near the ______. Physically, there is ___ difference between fog and a cloud. The basic difference is the ________and place of ___________. Clouds form when air rises and cools ____________. Fog forms from ________or the addition of enough water vapor to cause _____________. ground no method formation adiabatically cooling saturation

Radiation Fog Results from radiational cooling. Occurs at night. Requires clear skies and a high relative humidity The cold and dense air tends to flow downslope and is often thickest in mountain valleys After sunrise it dissipates (often said to “lift” or “burn off”). Fog evaporates from the bottom up (due to heating of the ground).

Advection Fog Results from warm air being blown over a cold surface. Common in San Francisco, Cape Disappointment, Washington, winter months in central eastern North America

Upslope Fog Rocky Mountains Formed when humid air moves up a gradual sloping plain or a steep mountain slope. The upward movement of the air causes it to expand and cool adiabatically. (This is the only type of fog that forms adiabatically.)

Steam Fog Arctic Sea Smoke Air just above warm water becomes saturated as cool air moves over it. Air has a “steaming” appearance and is shallow (it re-evaporates in unsaturated air above) Arctic Sea Smoke is steam fog formed in winter when cold air moves off continents and ice shelves of the north into the open ocean.

Dew and Frost Dew Frost below _______ Temperature next the ground cools to its dew point Water condenses on surfaces ________ Air temperature is _______ freezing. Deposition occurs on surfaces. Frost below

Precipitation: Moisture falling to Earth’s_________ from clouds. surface

Forms of Precipitation Rain __________ drops with a diameter of at least 0.5 mm (usually not larger than 5 mm) Often begins as ________ at high altitudes _________is composed of uniform droplets with diameters less than 0.5 mm. Liquid snow Drizzle

c. Snow Ice Crystals (1) ___________ that have grown as they traverse the cloud. (2) At temperatures greater than about -5o C, crystals usually stick together forming snowflakes

d. ________ Sleet Transparent or translucent, quasi-spherical ice (diameter less than 5 mm) Originate either as raindrops or snowflakes that have melted en route to the ground and are frozen as the move through a cold air layer near the ground.

e. ______________ (Also Called glaze ) Freezing Rain Rain or drizzle that freezes on impact with the ground or objects. Subfreezing air near the ground is not thick enough for liquid drops to freeze although the liquid drops become supercooled.

F._______: Formed in large cumulonimbus clouds Hail Small balls or chunks of ice with a diameter of 5 to 75 mm (largest on record fell in Coffeyville, Kansas on Sept. 3, 1970 and was 140 mm in diameter ). Produced by successive accretion of water drops around a small kernel of ice moving through a thick cloud. Produces several layers resulting in an onion-like cross section

3. Measuring Precipitation a. Rainfall Standard Rain Gauge

Tipping Bucket Rain Gauge

b. Snow Records ___________ is measured _______equivalent is determined 10 inches of snow = 1 inch of rain Snow depth Liquid

5. Weather Radar (1) Specific wavelengths are reflected by larger raindrops, ice crystals, or hailstones (penetrate small cloud droplets. (2) Echo results (reflected signal)

Radar Images Doppler Radar Conventional Radar