overview of the climate system
DESCRIPTION
Overview of the Climate System. Definition of climate Climate system components Earth’s energy balance & the greenhouse effect Water and carbon cycles Internal variability vs. forced variability (ENSO example) Natural forcings vs. human-induced forcings. Raymond Najjar - PowerPoint PPT PresentationTRANSCRIPT
Overview of the Climate System
Raymond NajjarPenn State Department of
Meteorology• Definition of climate
• Climate system components
• Earth’s energy balance & the greenhouse effect
• Water and carbon cycles
• Internal variability vs. forced variability (ENSO example)
• Natural forcings vs. human-induced forcings
Climate of a region:
Statistical description of that region’s weather
PortlandsWinter temperature probability distributions
Portland, ME(43.7°N)
Portland, OR(45.5°N)
Source: NWS Climate Prediction Center
Factors affecting a region’s climate
• Latitude• Elevation• Proximity to ocean• Prevailing wind direction• Atmospheric composition• Land surface type
Visible image Infrared image
Minneapolis
Source: Nese and Grenci (2010)
Minneapolis
Source: CLIVAR Program
Source: Wallace and Hobbs (2006). Based on Earth Radiation Budget Experiment (ERBE), 1985-1986
Source: Wallace and Hobbs (2006). Based on Earth Radiation Budget Experiment (ERBE), 1985-1986
Source: Wallace and Hobbs (2006). Based on Earth Radiation Budget Experiment (ERBE), 1985-1986
Average = 30 W m-
2 (warming)
Shortwave forcing average = 50 W m-2 (cooling)
Net effect: clouds cool 20 W m-2 Source: National Research Council (2008)
Global energy balance
Source: Kiehl & Trenberth (1997)
IR radiative forcing of the climate
IR radiation leaving the surface that is absorbed in atmosphere = 390 W m-2 – 235 W m-2 = 155 W m-2
Cloud IR forcing = 30 W m-2
Greenhouse gas forcing = 125 W m-2
Absorptivity of gases in the atmosphere
solar radiation terrestrial radiation
Dominant Dominant greenhougreenhouse gasse gas
Increasing due to human activity
Sources: Nese & Grenci (2010), Kiehl & Trenberth (1997)
60%
26%
8%
6%
Contribution to GHG forcing
Calculation of surface temperature without greenhouse forcing
Energy in = Energy out
Incoming solar = reflected solar + outgoing IR
1366 W m-2 = (0.30)(1366 W m-2) + 4T4
T = 254 K = -19° C = 2° F
Greenhouse effect warms surface ~60° F
The global water cycle
Source: Trenberth et al. (2007)
The global carbon cycleBlack = preindustrial, Red = 1990s change
Denman et al. (2007)
CO2 role in greenhouse effect
• ~ 25% of clear-sky greenhouse effect• ~ 20% of total greenhouse effect
• ~ 0.06% of the mass of the atmosphere
Forced vs. internal variability of climate
• Forced: due to “external” processes; e.g. solar, volcanic, & humans
• Internal: unforced variability; e.g. ENSO, NAO, PDO, AMO, etc.
Current conditions in the Tropical Pacific
Source: www.pmel.noaa.gov/tao
Source: www.pmel.noaa.gov/tao
Temperature section in the Equatorial Pacific
Source: www.pmel.noaa.gov/tao
Source: Nese and Grenci (2010)
ENSO variability over the past 60 years
MEI computed from surface winds, surface air and water temperature, and cloud fraction
Source: www.esrl.noaa.gov/psd/enso/mei/
Natural vs. Human-induced forcing of climate
• Natural: solar, earth-orbital, volcanic• Human-induced: land use change,
greenhouse gases, aerosols, soot
Discussion
ReferencesDenman, K.L., Brasseur, G., Chidthaisong, A., Ciais, P., Cox, P.M., Dickinson,
R.E., Hauglustaine, D., Heinze, C., Holland, E., Jacob, D., Lohmann, U., Ramachandran, S., da Silva Dia, P.L., Wofsy, S.C., Zhang, X., 2007. Couplings between changes in the climate system and biogeochemistry. In: S. Solomon, D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, T. Tignor, H.L. Miller (Editors), Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.
Kiehl, J.T., Trenberth, K.E., 1997. Earth's annual global mean energy budget. Bulletin of the American Meteorological Society 78, 197-208.
National Research Council Committee on Scientific Accomplishments of Earth Observations from Space, 2008. Earth Observations from Space: The First 50 Years of Scientific Achievements. The National Academies Press, Washington, D. C., 142 pp.
Nese, J.M., Grenci, L.M., 2010. A World of Weather: Fundamentals of Meteorology, Fifth Edition. Kendall Hunt Publishing Company, Dubuque, Iowa, 794 pp.
Trenberth, K.E., Smith, L., Qian, T., Dai, A., Fasullo, J., 2007. Estimates of the Global Water Budget and Its Annual Cycle Using Observational and Model Data. Journal of Hydrometeorology 8, 758-769.
Wallace, J.M., Hobbs, P.V., 2006. Atmospheric Science: An Introductory Survey, Second Edition. Elsevier, Inc., Oxford, UK, 483 pp.
Extra slides
Source: Global Carbon Project, www.globalcarbonproject.org/carbonbudget
CO2 emissions from human activity (black) compared with the rate of increase in
atmospheric CO2 (blue)
Source: Global Carbon Project