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Seasonal Change in the Upper Ocean (The Annual Cycle)

Seasonal Change in the Upper Ocean (The Annual Cycle). ● Amplitude Equator: 1 o -2 o C Mid-latitudes (40 o ): 5 o -10 o C Poleward: Reduced (melting and freezing of sea ice) Coastal region: 10 o -20 o C ● Evolution Northern hemisphere Maximum SST: August/September

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Seasonal Change in the Upper Ocean (The Annual Cycle)

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  1. Seasonal Change in the Upper Ocean (The Annual Cycle)

  2. ● Amplitude Equator: 1o-2oC Mid-latitudes (40o): 5o-10oC Poleward: Reduced (melting and freezing of sea ice) Coastal region: 10o-20oC ● Evolution Northern hemisphere Maximum SST: August/September Minimum SST: February/March Sub surface: Delayed up to 2 months. ● Annual cycle decreases rapidly with depth: confined mostly above 100 little change below 200 meters SST Annual Cycle Departure of monthly climatology from climatological annual mean (based on CPC data, 1982-2001)

  3. Annual cycle of temperature in the upper layer Mixed layer: In winter, SST is low, wind waves are large, mixed layer is deep (extending to the main thermocline). In summer, (SST highwater stable), mixed layer is shallow. Seasonal thermocline: seasonal thermocline develops in the upper zone in summer. high stability within the seasonal thermocline separate the water from upper to deeper zones causing a “fossilized mixing zone” (water from remaining winter mixed layer) Example: Seasonal thermocline at Ocean Weather Station “P” (50oN, 145oW) March is nearly isothermal in upper 100 meters. March-August, SST increases, (absorption of solar radiation). Mixed layer  30 m. August-March, net loss of heat, seasonal thermocline eroding due to mixing.

  4. Seasonal change of temperature profiles at different latitudes

  5. Temperature diurnal cycle • SST diurnal cycle: usually small(<0.4oC) • Diurnal cycle is mainly in upper 10 meters • Produce a “diurnal thermocline” • Localized higher amplitude: 1oC (occasionally 3o-4oC) in regions of high isolation + low wind, 2~3oC in shallow water along coast.

  6. Seasonal Cycle of the Thermocline at Equatorial Atlantic Ocean

  7. Some Examples of the Interannual Variability in Upper Tropical Ocean

  8. Standard deviation of SST anomalies

  9. Fluctuations of the equatorial undercurrent and thermocline depth during 1981-1983

  10. An example of El Niño evolution

  11. December,1997-February, 1998 20oC isotherm anomalies (m) COLA ODA SSH anomalies (cm) TOPEX/Poseidon

  12. Tropical Atlantic SST Anomalies

  13. ENSO-like phenomenon is not just found in the Pacific

  14. Anomalous event in the Indian Ocean

  15. And not just the tropics Image courtesy of Stepen Hare and Nathan Mantua, University of Washington, units are degrees Celsius The Pacific Decadal Oscillation (PDO) is a long-term ocean fluctuation of the Pacific Ocean. The PDO waxes and wanes approximately every 20 to 30 years.

  16. And it is not just ENSO!

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