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Ocean and ClimateAn Introduction
Program in Climate Change Summer InstituteFriday Harbor Labs
16-18 September 2008
Dennis L. HartmannAtmospheric Sciences
University of Washington
Ocean and ClimateAn Introduction
• Role in Earth’s Evolution
• Role in Climate Change - Past & Future
• Impact of Ocean Change - e.g. sea level.
• Impact of Human Activities and Climate Change on the Ocean - e.g. acidification.
Basic Properties• The Ocean is Dark - low albedo• The Ocean is Wet - Cools by Evaporation• The Ocean is a fluid with mass/heat capacity
– Can store and release energy quickly (or slowly)– Can move energy around – Can store and release trace chemicals (e.g.CO2)
• The Ocean can freeze, in which case it is a bright solid and energy transfer by phase transition is less important (sublimation).
Ice-Albedo Feedback
• As the Earth warms, ice melts in high latitudes and altitudes
• This lowers the albedo of Earth and leads to further warming.
• Ice reflects more solar radiation than other surfaces
Ice-Albedo Feedback
• As the Earth warms, ice melts in high latitudes and altitudes
• This lowers the albedo of Earth and leads to further warming.
• Ice reflects more solar radiation than other surfaces
Tropical SST and Clouds
• Distribution of tropical SST is hypothesized to have strong effect on clouds and the energy balance.
• For example, marine boundary layer clouds have strong leverage on the radiation balance and depend on the strength of the trade winds and SST gradients.
• Cover a significant fraction of the Earth’s Surface
• Have a large effect on Earth’s Energy Budget
Cloud Forcing of the Energy BalanceCloud Forcing of the Energy Balance
-70 0 +30 Wm-2-30
Ocean a Source/Sink of radiatively active gases and
aerosols.• Carbon uptake/release
– Glacial/Interglacial– Anthropogenic Carbon uptake - 50%
• DMS production - Sulfate Aerosols/CCN• Sea Salt Aerosols
The atmospheric concentration of CO2 and CH4 in 2005 exceeds by far the natural range of the last 650,000 years
CO2
CH4
The Ocean Freezes, or not- Sea Ice
• Freezing of seawater an important driver of thermohaline circulation.
• Sea Ice + Snow = insulation• Large albedo increase .• Polar amplification and seasonal
dependence of polar warming - largest polar warming in winter.