PDF-Clouds types for observations

IB 7A pAA703 6E3D3 B 2347n3 77B32 nC03 4 161B37AB71 4A 0A3D32 D3 B63 E2 7nB E6716 1C2A 1n 03 02G 5Cp32 T63 2 M3B3571 O5n7HB7n MO 6A 2En Cp 1AA7471B7n 4 B63A3 161B37AB71 4A B 3n03 n 0A3D3 B 3pB B63 BGp3A 4 1C2 p3A3nB T67A pC071B7n 7CABB3A n2 3Fp7nA. Robert Wood. , Matthew . Wyant. , Christopher S. . Bretherton. , Jasmine . Rémillard. , . Pavlos. . Kollias. , Jennifer Fletcher, Jayson . Stemmler. ,. . S. . deSzoeke. , Sandra . Yuter. , Matthew Miller, David . Dea Doklestic . G&G 570 Class . Project. Heat Budget Group Presentation, June 16, 2011. Questions. How do clouds influence surface heat budget?. How are turbulent heat fluxes influenced during overcast conditions?. Second Grade Science. By: Christy Gibson . Clouds. A . cloud is composed of tiny water droplets (or ice crystals) that are suspended in the air. . If . the droplets become large enough. , they . may be visible as a cloud or fog. Two key impacts. Cloud feedback. Response of clouds to increased CO. 2. Aerosol indirect effects (AIEs). Response of clouds to changes in aerosol particles. Cloud feedbacks. Uncertainty in cloud feedbacks is main source of uncertainty in climate sensitivity. What is a cloud?. A cloud is a group of water droplets in the atmosphere.. The water vapor condenses during the water cycle to form clouds.. Cirrus Clouds. They are the highest clouds.. They look thin, wispy, or feathery.. By Kelsey Shields. Definition. A cloud is a visible collection of particles of ice or water suspended in the air, usually at an elevation above the earth’s surface.. Different Kinds. There are four different types of clouds families. We then break the four families into ten different genus. They differentiate in the way they look, and the level of height they are at.. Notes/Vocabulary. How do clouds form?. when warm air & cold air meet, cold air pushes up the warm air and a cloud can form. when air rises and cools, the water vapor in the air condenses into tiny water droplets and forms a cloud. The SOCRATES Planning . Team. : . Greg . McFarquhar. (. mcfarq@atmos.uiuc.edu. ),. Roj. . Marchand. , . Robert . Wood, Chris . Bretherton. , Alain . Protat. , Patricia Quinn, Steven . Siems. , Simon Alexander, and Bob Weller. Cumulus Clouds. Cumulonimbus Clouds. Stratus Clouds. MSI-CIEC All Hands Meeting. SDSC January 27 2010. Geoffrey Fox. gcf@indiana.edu. . . http://www.infomall.org. . http://www.futuregrid.org. . Director, Digital Science Center, Pervasive Technology Institute. Michael . Armbrust. Armando Fox. Rean. Griffith. Anthony D. Joseph. Randy H. Katz. Andrew . Konwinski. Gunho. Lee. David A. Patterson. Ariel . Rabkin. Ion . Stoica. Matei. . Zaharia. Electrical Engineering and Computer Sciences. Cirrus clouds can best be described as “ice-crystal” clouds that look like wispy curls of hair. These clouds are often the first signs of approaching weather changes. . Cirrus. These clouds are often referred to as “mackerel sky”. The ripples in these clouds look like the scales on a fish and are a sign of unsettled weather to come. . . SYFTET. Göteborgs universitet ska skapa en modern, lättanvänd och . effektiv webbmiljö med fokus på användarnas förväntningar.. 1. ETT UNIVERSITET – EN GEMENSAM WEBB. Innehåll som är intressant för de prioriterade målgrupperna samlas på ett ställe till exempel:. Clouds. Form when air rises, cools to its dew point, and becomes saturated. Shape and height of clouds vary with temperature, pressure, and water vapor in atmosphere. Clouds. Shape. Stratus-smooth, even sheets or layers at low altitudes.