TOPIC:-TYPES OF PRECIPITATIONS PROJECT REPORT BY: - MINTU.R.PATEL ENROLL NO.:- 126310306509 GUIDED BY: - F.P.AMBADIA V.B.PATEL M.M.SHAH TOPIC: - TYPES OF PRECIPITATIONS Sr.No. Date Title Page No. (1) 5/3/2014 INTRODUCTION 3 (2) 5/3/2014 Convective precipitation 3 (3) 5/3/2014 Orographic precipitation 4 (4) 5/3/2014 Cyclonic precipitation 5 (5) 5/3/2014 Frontal precipitation 6 (6) 5/3/2014 Precipitation due to turbulent
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Terre Haute‚ Indiana Johnny L. Luckett Excelsior College Abstract This paper discovers the water budget for Berkeley‚ California in comparison to Terre Haute‚ Indiana. The two cities precipitation differs throughout the twelve month calendar year where many of the heavy precipitation months are totally opposite. Berkeley California’s winters‚ where the majority of rain occurs and Terre Haute‚ Indiana where the rainfall is observed as consistently disseminated throughout the year
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CLIMATOGRAMS: Table 16: Chaparral Table 17: Tropical Deciduous Table 18: Tropical Desert Table 19: Boreal Forest Table 21: Tundra ANALYSIS: 1. Yes; each biome has very distinct characteristics pertaining to temperature and precipitation. Temperature‚ depending heavily on the latitude of the biomes‚ was typically higher in tropical areas that are clearly closer to the
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America are from Portland‚ Oregon to all of California (www.eoearth.com). The average temperature of the coldest month is less than 18°C (64°F) but above -3°C (27°F). The wettest winter month has about 3 times more precipitation when compared to the driest summer month. Precipitation in driest summer month is less than 40 mm (1.6 in.). Warmest month has average temperature above 22°C (72°F) and at least 4 months have average temperatures above 10°C (50°F).
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.6Name: Danielle Hall|Date: 10.15.2012| Exp 9: Stoichiometry of a Precipitation Reaction|Lab Section: | Data Tables: Step 3: Show the calculation of the needed amount of Na2CO3 CaCl2.H2O(aq)= m/M =1/147 =0.0068 mol CaCO3(s)=0.0068*1/1 =0.0068 mol CaCO3(s)= CaCO3 (s)= CaCO3 mol *CaCO3 g =0.0068 mol*100.01 g =.68 g Step 4: Mass of weighing dish _0.6___g Mass of weighing dish and Na2CO3 __0.72__g Net mass of the Na2CO3 ___0.12_g Step 6: Mass of filter paper
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decreased a little‚ but the dew point dropped significantly. Suddenly‚ on the 30th‚ dew point shot up to equal the temperature. Every time that the dew point was near the temperature‚ there was a higher chance of precipitation. For example‚ on the 4th‚ 6th‚ 7th‚ 16th‚ and 30th‚ there was precipitation. On all of these dates‚ the dew point was close to the temperature. Also‚ the temperature trend was a decrease. This is probably because it was getting closer to winter and the angle of insolation was decreasing
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recent years‚ rain-dependent activities such as Agriculture in the tropical zone had been entirely dependent on the regular patterns and timing of the onset‚ amount and duration of the rains‚ people depended on their indigenous knowledge of these precipitation trends to predict the planting and harvesting seasons‚ nowadays‚ reliance on these native self-knowhow to plan agricultural activities and day to day chores has proven terribly mistaken; most studies has laid all the blame on climate change (global
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meant was that the overall Ocean Mixed-Layer Temperature went up and this of course affected the Precipitation and Snowfall levels directly. Background/Introduction: The objective of the assignment was to find out the comparisons of fluctuating levels from the years 1958 to 2062 in the Western United States and compare them to see if there was any change. The factors used for comparison were Precipitation‚ and Ocean Mixed-Layer Temperature. Problem: 1) What are the future Changes predicted by
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& coalescence precipitation process. Know the main premise of the ice-crystal (Bergeron) precipitation process. Chapter 5 Questions and Topics to Study (cont’d) Know the difference between freezing rain and sleet‚ including the type of lower atmosphere that can produce each of these types of winter precipitation. (Hint: See Active Figure 5.32 on page 139) How does Doppler RADAR measure the intensity of precipitation?
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Factors that affect climate Latitude: Ocean Currents: Wind and air masses: Elevation: Relief: Near water: Global Factors that Affect Climate As the suns UV rays hit the earth they hit is directly at the equator causing more heat. Because these rays are direct and they hit direct at one spot. For part a‚ the earth start to slope‚ in which the sun’s rays have to hit a larger areas‚ and have to travel further distances. As the latitude increases‚ the average annual temperatures decreases. In North
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