'Low clouds' diaporamas de présentation

WEAX-201 Chapter 6--Condensation, Dew, Fog, and Clouds

1.17k views • 69 slides

Cloud Formation

Cloud Formation. Matt Rogers ( rogers@atmos.colostate.edu) Department of Atmospheric Science Colorado State University AIM Workshop 25 July 2006 Anchorage, Alaska. Water Cycle Revisited. Sources of water for clouds come from evaporation and transpiration

1.15k views • 36 slides

Cloud Formation

Cloud Formation. Matt Rogers ( rogers@atmos.colostate.edu) Department of Atmospheric Science Colorado State University AIM Workshop 25 July 2006 Anchorage, Alaska. Water Cycle Revisited. Sources of water for clouds come from evaporation and transpiration

554 views • 36 slides

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

489 views • 34 slides

Clouds and Precipitation

Clouds and Precipitation. Lifting, condensation, and cloud development Deep convective clouds (thunderstorms) Types of clouds and how they form Collision and coalescence of raindrops Crucial roles of ice in most precipitation. Cloud Development. Clouds form as air rises, expands and cools

609 views • 32 slides

Unraveling the Life Cycle of Low Clouds

Unraveling the Life Cycle of Low Clouds. Mark A. Miller Rutgers University . Suppressed environments f avor low clouds Significant (but not overwhelming) subsidence Adequate BL water vapor Source of BL TKE Saturation beneath the inversion Shallow clouds dominate regardless the time of day

509 views • 32 slides

Size Comparison (picture of cloud droplet vs. rain droplet)

Size Comparison (picture of cloud droplet vs. rain droplet). Cloud Types Read 27.3. Know the Following Latin. Latin Root Translation cumulus heap stratus layer cirrus curl of hair nimbus rain. High Clouds (usually made of ice crystals). CIRRus CIRRocumulus CIRRostratus.

564 views • 29 slides

Moisture in the Atmosphere

Moisture in the Atmosphere. Mr. Ahearn Regents Earth Science 2009. Cloud Formation. Buoyancy is the tendency for air to rise or sink as a result of differences in density. Clouds form when warm, moist air rises, expands, and cools in a convection current.

386 views • 24 slides

Chapter 18

387 views • 21 slides

Fog, dew and clouds Meteorology 10 Prof. Jeff Gawrych

Fog, dew and clouds Meteorology 10 Prof. Jeff Gawrych. Dew: air cooled to dewpoint. Frost: air cooled to dewpoint, but temp is at or below freezing point. How can clouds form?. Air needs to be cooled to saturation. I.e. air cooled to dew point. I.e air reaches 100% RH

315 views • 19 slides

Lecture 12

267 views • 17 slides

Types of Clouds

Types of Clouds. Kristian Diore 3 r d Grade Science. Click here to begin!. Click on each cloud to learn more about it!. Cumulus clouds. Cirrus clouds. Stratus clouds. Nimbus clouds. Click here for a review question. Cumulus Clouds. Puffy, white clouds

3.2k views • 16 slides

Cloud Identification

559 views • 13 slides

Basic Cloud Types

597 views • 13 slides

U.S. Navy Meteorology and Oceanography Detachment Asheville, NC

288 views • 11 slides

5 am (12 Z) 7 Jan

5 am (12 Z) 7 Jan. Low clouds. 5 pm 7 Jan. almost a thin cloud here at top of Polluted gunk layer . Low clouds. ~Noon Jan 7 (low clouds are grey). Most of fog has dissipated over valley, thick Pollution remains. 7 January afternoon from Grandeur. 5 am 16 Jan.

224 views • 11 slides

Chapter 7: Feedbacks

Chapter 7: Feedbacks. GEO 307. P ositive feedback - initial change will bring about an additional change in the same direction. Example - growth of an interest-earning savings account. As interest is accrued the principal will begin to grow.

197 views • 9 slides

Air Masses and Fronts

205 views • 9 slides

Rusty Billingsley NWS Southern Region

Rusty Billingsley NWS Southern Region. Operational Enhancements by Leveraging the GOES-R Proving Ground. Questions posed:. How might satellite resources be more effective in helping provide operational products/services?

165 views • 8 slides

Understanding The Effects of The Great Salt Lake

Understanding The Effects of The Great Salt Lake. Great Salt Lake breeze fronts strengthen the low-level stability during CAPs. The Great Salt Lake modulates clouds and fog during CAPs. l ow clouds. fog. 7 Jan 2011 MODIS. Warm Salt Lake Valley air. Cold lake air. 27 Jan 2011 MODIS.

175 views • 1 slides