Ocean Atmosphere Notes 2 PDF

Formation of mid-latitude cyclone Elman transport convergence - counterclockwise N. Hemi -oncestable stratificationne...

Formation of mid-latitude cyclone Elman transport convergence - counterclockwise N. Hemi -oncestable stratificationne o = Surface Divergence 4 Surface Convergence Gyres = current system seasurface -) water converges in gyre Centre downwelling ↑ - upwelling s S ↓ STG A Thermocline E Thermocline STG Orographic Lifting Rain Shadow Relative humidity · STG STG STG. RH = potial presse x100 - vapour pressure Ac AAC --- STG = Subtropical Gyre air generates Rising e SPG Subpolar Gyre which precipitation = low pressure , AAC = arctic currents leads to ocean currents are driven by wind direction? But why do they not move in the same · Coriolis Force to the wind in Northern deflects water right of esset hemisphere to the left of wind in Southern deflects water CN Hemil. hemisphere wind direction terrain and rises Ekman Transport > ① wind hits mountain - ↓ warm which relatea surface altitude layer net water movement air cools as it gains , precipitation creating clouds + humidity to 100 % Heri and S ③ depleted of moisture sinks. cold air warm dry air , RH decreases becomes porcote so deflects each layer , a coridis effect Rh = x does friction coriolis is result of shear stress , , ekman spiral a and water drag with the ocean floor is created by friction Shear stress drift icebergs do not observed when Fridtjof noticed of the wind in the same direction and Left in S Hemi in N Hemi. to the Coriolis acts right. ↓Pry first to explain this process Eman was the Fridtjofs student , shear stress moves bottom room sur face wind moves , 12 drives subtropical gyres I ↑ peesterlies 2 ↓ I ↳ Des -Northeast ~ - Coding Also ↑ the be of expansion ↓-esterlies -10/1000m = Heating be of condensation Dr = + 50/1000m seeselling WetRate has to be rising a WestpiegingLow =