280 likes | 412 Views
MPO 551, Class 2. http://www.tstorms.org/tropical-storms/. MPO 551, Class 2. $$$1.00$$$ to Andrew - p.23. “ air circulates counterclockwise around Lows [in the NH] and counterclockwise around Highs”. The Earth System: The oceans, cryosphere, Hydrologic cycle Carbon cycle Oxygen
E N D
MPO 551, Class 2 http://www.tstorms.org/tropical-storms/
$$$1.00$$$ to Andrew - p.23 “air circulates counterclockwise around Lows [in the NH] and counterclockwise around Highs”
The Earth System: • The oceans, cryosphere, • Hydrologic cycle • Carbon cycle • Oxygen • Earth’s history
WATER: Mass in units of 103 kg m-2 ~ 100 cm deep The oceans: 72% of earth’s surface, 97% of the earth’s Non-geologic water. Ice sheets ~ 2%, and 80% of earths Freshwater. Antarctica ~ 89% of ice mass, Greenland 9%, Surface area also important.
Role of Oceans in Climate: • thermal inertia • heat transport • El Nino • uptake of carbon • source of trace gases
Ocean Temperature: Thin, mixed surface layer + thermocline + deep layer
M-AERI Observations The Marine & Atmospheric Emitted Radiance Interferometer precisely measures the temperature of the ocean’s thin surface layer or skin. Temp (°C) Day of the Year 2003
Time evolution of near-surface thermal gradients SkinDeEP profiles on 12 October 1999.Off Baja California, R/V Melville. From Ward, B. and P. J. Minnett, 2001. An autonomous profiler for near surface temperature measurements. Gas Transfer at Water Surfaces. M. A. Donelan, W.M. Drennan, E.S. Saltzmann and R. Wanninkhof (Eds.) American Geophysical Union Monograph 127. 167 - 172.
Surface height anomaly SST, 8/27/05 Tropical cyclone heat potential Depth of 26.5 C isotherm Gustavo Goni (AOML) Joaquin Trinanes (CIMAS)
Ocean composition: ~ 35 g/kg dissolved salts,or 35 0/00, parts per thousand by mass Denser than fresh water by ~2.4% Density gradient = pycnocline Temperature change required to offset change in salinity of 1 g/km, as f(T)
Wind drift & sea level annual Wind drift and TOPEX sea-level
Costa Rica shallow thermocline dome S.-P. Xie, TRMM SST + precipitation, 5-year average
Annual mean SST SST Departure from zonal-mean
Globally, P ~ E over continents, P>E Winds+water vapor TRMM
Sheba track Winter arctic sea-ice motion, from buoys. Beaufort Gyre.