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Posted: Thu Jul 07, 2022 1:34 pm
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C +0 session masteringgeology.com/yt/hm/wathb1682854 Mastaring Assignments Give It Some Thought: Air Temperature and its Relationship with Elevation and Dew Point Part A temperature and pricelevation pe Dew post chang Cudsen Arno obove t the Ye 7 VA 4 km 3 km 2 km 1 km Windward tamat Type festuari LIFE 3PC Otevbert batter are re D en bege of 1900 was fo Leeward lary dat w pawe to zadan 10.4. The promena 3ds > desten 240 !
ant Mahogy Mahering x session/masteringgeology.com/my/meignmoblem-166208548offatt с ring Assignment It Some Thought: Air Temperature and its Relationship with Elevation and Dew Point Drag the appropriate tabels to their respective targets View Available H 17 5 3 km 2 km 1 km Seo level T₂ IPC T₂-TCTCT-CT-170 Windward 1 Q A 2 N W S Temperature of Point A - 27C Dew point temperature at Point A 17C Dew point temperature at Point D-7C Dry adiabatic rete 10 CAM Wet adobatic rate SCA 3 W E O X S D 4 R C F T 6 Leeward Idry at G 4. 7 B H dat Mel 6
4 km 3 km 2 km 1 km Sea level Thit = 7°C Windward (wet climate) Tair=12°C A Tair = = 37°C Tair = 27°C Tair=17°C Leeward (dry climate) U Temperature at Point A = 27°C Dew point temperature at Point A 17°C Dew point temperature at Point D = 7°C Dry adiabatic rate 10'C/km Wet adiabatic rate= 5'C/km Reset
Catering Assignment Give It Some Thought: Air Temperature and its Relationship with Elevation and Dew Point Part A-Art and price M As slave Drag the appe YAHONDA PAGE D www. SME))
nt Mastering Geology MasteringO x session.masteringgeology.com/myct/itemView?assignment ProblemID=168288 ng Assignment 9 Some Thought: Air Temperature and its Relationship with Elevation and Di Part A - Air temperature and topographic elevation The diagram below shows ar flowing from the ocean over a coastal mountain range • As elevation increases, air temperature decreases Dew point changes with elevation Al point A, the dew point is 17°C. On the windward side, the • Clouds begin to form once they meet the mountain range front (windward side) Here, humidity Air temperature change on the windward side of the range follows the wet adiabatic rate, but not Ar temperature above the dew point and on the leeward side can be predicted using the dry adi Use this information to determine the air temperature at points 6 through G on the diagram Each point graphic is useful for answoning the question, especially the dry and wet adiabatic rates Drag the appropriate labels to their respective targets View Available Hints) 4 km Windward twet climate 3 km PType here to search 2 . O B
eases until it reaches 7°C at point D. The dew point is constant at 7C on the leeward side reaches a 100% concentration in the air, meaning the dew point is on the windward side point is reached change in height of 1000 meters Poet B, for example, is 1000 m higher than point A The information Reset Help Ban Leeward try climate) Ⓡ 73 99°F P 17 < N 10