'Cold clouds' presentation slideshows

1.02k views • 71 slides

Midterm Exam #2 Tuesday, March 23

Midterm Exam #2 Tuesday, March 23. Closed book Will cover Lecture 8 (Special Relativity) through Lecture 14 (Star Formation) only If a topic is in the book, but was not covered in class, it will not be on the exam! Some combination of multiple choice, short answer, short calculation

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AOSC 200 Lesson 8

AOSC 200 Lesson 8. Precipitation Growth in Warm Clouds. Cloud droplets are typically 10 microns in size. small raindrops are typically 1000 microns (almost one million droplets) How does one go from one to the other?

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Spectral Line Survey with SKA

Spectral Line Survey with SKA. Satoshi Yamamoto and Nami Sakai Department of Physics, The Univ. of Tokyo Tomoya Hirota National Astronomical Observatory of Japan. Interstellar Chemistry. Various new research fields in chemistry. A useful tool to study star formation processes. .

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MODIS CLOUD RETRIEVAL: A presentation based on this document.

MODIS CLOUD RETRIEVAL: A presentation based on this document. MODIS ATMOSPHERE PRODUCTS. Basic Idea Behind Cloud (and Snow) Retrievals. Pg 9. Spectral Extinction Coefficient for Water Droplet Cloud: Refractive Index Effects.

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Clouds

Clouds. By: CeCe, Maggie, and Jordan First Period. How are clouds formed?. Water evaporates from oceans, lakes, rivers, and streams as well as small pools of water. Air has to be a little bit dirty for a cloud to form. High amounts of humidity helps form clouds.

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ATOC 4720 class19

ATOC 4720 class19. Thunderstorms 1. Growth of clouds droplets in warm and cold clouds 2. Charge generation 3. Lightning and thunder . 1a. Growth of droplets in warm clouds. Clouds lie completely below. warm clouds;. Droplet grow: (1) condensation in

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Forms of Precipitation

Forms of Precipitation Rain liquid form often originates as snow drizzle smallest diameter of raindrops Snow ice crystals density much less than rain 1 inch rainfall = 10 inches snow (avg) Forms of Precipitation, cont. Sleet frozen raindrops

4.61k views • 8 slides

PRECIPITATION

PRECIPITATION. Equilibrium- inbound cloud droplets equal the outbound cloud droplets. Condensation- inbound cloud droplets exceed outbound cloud droplets. Evaporation- inbound cloud droplets are less than outbound cloud droplets. Cold Clouds from above the freezing level. Freezing Level.

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