'Middle clouds' presentation slideshows

CHAPTER 10 ICING

CHAPTER 10 ICING. ICING. Aircraft accidents generally occur after a series of events place a pilot in a box from which he cannot escape. Having knowledge of icing and how it affects your aircraft may prevent the last side of the box from closing. Ice is a Cumulative hazard. HOMEWORK.

1.43k views • 63 slides

ESCI 241 Meteorology

ESCI 241 Meteorology. Cloud Identification. Divergence. High Clouds. Cirrus. Cirrocumulus. Cirrostratus. Middle Clouds. Altocumulus. Altostratus. Low Clouds. Stratus. Stratocumulus. Nimbostratus. Clouds of Vertical Development. Cumulus Humilis. Cumulus Congestus. Cumulonimbus.

678 views • 52 slides

Understanding Weather and Climate 3rd Edition Edward Aguado and James E. Burt

489 views • 34 slides

527 views • 31 slides

Types of Clouds

Types of Clouds. A fifth grade Powerpoint slide show. created by Mrs. Sheehan 1/07. Most clouds you see in the sky are based on these three basic cloud types:. Cumulus - puffy, like a cotton ball Stratus - flat, covers the sky like a blanket Cirrus - high, wispy clouds.

460 views • 30 slides

Temperature and pressure

Temperature and pressure. Remember: Temperature is the average speed of molecules. Predictions: What do you think happens to Pressure as Temperature Increases? What do you think happens to Pressure as Temperature Decreases?. Temperature, pressure, and density.

561 views • 18 slides

Extending HIRS High Cloud Trends with MODIS Donald P. Wylie Richard Frey Hong Zhang

Extending HIRS High Cloud Trends with MODIS Donald P. Wylie Richard Frey Hong Zhang W. Paul Menzel 12 year trends Effects of orbit drift and ancillary Tsfc Comparison with MODIS July 2002. Cloud Properties from CO2 Slicing

288 views • 18 slides

Moisture in the atmosphere

Pg. 71. Moisture in the atmosphere. Cloud formation. The tendency to rise or sink because of differences in density is called buoyancy Clouds form when warm, moist air rises, expands, and cools around condensation nuclei. Condensation nuclei mainly form from dust and salt

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Basic Cloud Types

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Cloud Identification

560 views • 13 slides

297 views • 13 slides

Basic Cloud Types

597 views • 13 slides

Welcome Gallery Owners

Welcome Gallery Owners. Low Clouds. Stratus, Stratocumulus, Nimbostratus: Ground to 2000 Meters: Water Droplets. Middle Clouds. Altostratus, Altocumulus. 2000-8000 Meters: Ice Crystals and Water Droplets. High Clouds. Cirrus, Cirrostratus, Cirrocumulus 6000-18000 Meters: Ice Crystals.

248 views • 13 slides

How can clouds form?

How can clouds form?. Air needs to be cooled to saturation. I.e. air cooled to dew point. I.e air reaches 100% RH As air rises, it cools * How to force air to rise: Topography fronts convection Convergence ---> <---- 2) Surface cools off quickly by emitting radiation

197 views • 9 slides

Clouds

Clouds. Cloud Formation. Moist air rises Convectional lifting: warm air is less dense than cold air Orographic lifting: when wind encounters a mountain, the air must go up. . Cloud Formation. Air expands and cools Cooled water vapor condenses Cloud droplets form

275 views • 8 slides

Clouds: Types & Formation

Clouds: Types & Formation. Meteorology. Warm moist air rises, expands, and cools in a convection current Air reaches dew point, water vapor in air condenses around small particles in atmosphere (sea salt, dust) Millions of these droplets collect= form clouds

223 views • 7 slides