'Climate forcing' presentation slideshows

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Lecture #1

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Climate Forcing Factors in Earth History

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Inez Fung University of California, Berkeley

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Climate Change

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Activity for Dec. 5 (last 20 points)

Activity for Dec. 5 (last 20 points). How far did your food travel?. Activity for Dec. 5 (last 20 points). How far did your food travel? Choose a meal. Activity for Dec. 5 (last 20 points). How far did your food travel? Choose a meal. Record calories for all items in your meal.

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Emissions of greehhouse gasses

Emissions of greehhouse gasses. Climate forcing factors = Factors causing climate to change. Temperature. Direct temperature measurements span 140 years. Global temperature has increased about 1 deg C. Some solar radiation is reflected by atmosphere. Sun.

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CORDEX South Asia: A framework for addressing regional monsoon issues in a changing climate

CORDEX South Asia: A framework for addressing regional monsoon issues in a changing climate R. Krishnan, T.P. Sabin, J. Sanjay, M. Mujumdar, P. Priya, M.V. Rama Rao, Sandip Ingle, V. Ramesh, Madhura Kane Centre for Climate Change Research Indian Institute of Tropical Meteorology, Pune.

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CORDEX South Asia: A framework for addressing regional monsoon issues in a changing climate

CORDEX South Asia: A framework for addressing regional monsoon issues in a changing climate R. Krishnan, T.P. Sabin, J. Sanjay, M. Mujumdar, P. Priya, M.V. Rama Rao, Sandip Ingle, V. Ramesh, Madhura Kane Centre for Climate Change Research Indian Institute of Tropical Meteorology, Pune.

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Detail of time-stratigraphic record in ice cores

Detail of time-stratigraphic record in ice cores. In some cores, where accumulation rate is high, sub-annual (seasonal) records are preserved Allows exact age determination of ice, for thousands of years in the past. GISP 2D, 2114 m. Holocene. 115KYBP.

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Climate Change Research Division

Climate Change Research Division. BERAC Spring meeting May 20, 2008. Climate Change Research Division. DOE Climate Change Research Program Budget. FY 2008 Budget, $M ARM Research $14.8

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We are now acting because the risks of inaction would be far greater.

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OUEVRE (Per Jonsson, revisions by F. Werner

OUEVRE (Per Jonsson, revisions by F. Werner. What have we learned? What models (or other approaches to synthesis) exist or are needed and of what type? How does climate influence variability of recruitment in these systems?. Model Resolution-Temporal/Spatial Issues of Model Integration.

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We are now acting because the risks of inaction would be far greater.

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HFCs: A Critical Link in Protecting Climate and the Ozone Layer

HFCs: A Critical Link in Protecting Climate and the Ozone Layer. A. R. Ravishankara Guus Velders Melanie Miller Mario Molina. Steering committee headed by Joseph Alcamo. Disclaimer: I am not talking as a co-Chair of WMO/ENEP SAP panel

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Weather/Climate services

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Two kinds of geoengineering

1. Two kinds of geoengineering. Solar radiation management (SRM) Sulfates in the stratosphere to mimic volcanoes Sea salt aerosols to make low-altitude clouds brighter or more common Making crops more reflective Reducing high-altitude cirrus clouds. Carbon cycle engineering (CDR)

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Global Warming Effects of increase CO 2

Global Warming Effects of increase CO 2. Carbon dioxide. Can we be completely sure that the climate changes we observe are caused by anthropogenic emissions of carbon dioxide?. But it is likely :. Climate Models Predictions. What do climate models lead us to expect?.

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