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Global Climate Change: Global Climate Change: Causes and Consequences Causes and Consequences Anthony J. Broccoli Director, Center for Environmental Prediction Rutgers University [email protected] Delaware Estuary Science Conference Cape May, NJ January 24, 2007

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Page 1: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Global Climate Change:Global Climate Change:Causes and ConsequencesCauses and Consequences

Anthony J. BroccoliDirector, Center for Environmental Prediction

Rutgers [email protected]

Delaware Estuary Science ConferenceCape May, NJ

January 24, 2007

Page 2: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the
Page 3: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the
Page 4: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the
Page 5: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Coupled Climate Model Schematic

Page 6: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Variations among colored bars represents uncertainty due to uncertainty in future emissions.

Height of each colored bar represents variations among different climate models.

Page 7: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Potential Climate Change ImpactsPotential Climate Change Impacts

Page 8: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Coastal Environment

Water Resources

Page 9: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Sea Level Trends in New Jersey

Atlantic City, NJ

Source: National Oceanic and Atmospheric Administration

Page 10: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Why Is Global Sea Level Rising?

Thermal Expansion:Warmer water is less dense

than colder water.

The ocean has been gaining heat.

Page 11: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Why Is Global Sea Level Rising?

Melting Glaciers and Ice Caps:

Water released by the melting of ice on land adds to the volume of the oceans.

Source: Roger Braithwaite, Univ. of Reading

Page 12: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Changes in Glacier Mass

Page 13: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Effects of Sea Level Rise on the Coastal Environment

Land area susceptible to inundation

Land area susceptible to coastal flooding

50% probability of 0.61 m SL rise by 2100

1% probability of 1.22 m SL rise by 2100

from M. D. Beevers, Princeton University and Univ. of Maryland

Page 14: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

“Ash Wednesday Storm”

Harvey Cedars, March 1962

Page 15: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Effects of Climate Change on Water Resources: Floods and Droughts?Cannonsville Reservoir, Dec. 2001

Delaware River, Sept. 2004

Easton-Phillipsburg BridgeJune 2006

Page 16: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Discharge at Flood Stage

Page 17: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Global Warming and the Hydrologic Cycle

• The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the surface is balanced by evaporation and sensible heating of the atmosphere.

• If the downward flux of energy increases, then evaporation will increase.

• On a global basis, evaporation and precipitation must balance.

• Thus as the earth warms, both evaporation and precipitation will increase.

Page 18: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Annual mean rainfall rate change(2071-2100) minus (1961-1990), mm/day

Source: IPCC Working Group I (2001)

Page 19: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Delaware River Salt Front

Late Jan. normal

Drought of Record

Source: Delaware River Basin Commission

Page 20: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

More Warming in the Pipeline?

Future emissions

Additional “zero-emission”warming (aka “commitment”)

Warming to date

Page 21: Global Climate Change: Causes and Consequences · Global Warming and the Hydrologic Cycle • The downward flux of radiative energy (i.e., sunlight and infrared radiation) at the

Managing Climate Change

• Mitigation: Reduce emissions of carbon dioxide and other greenhouse gases.

• Adaptation: Increase the resilience of society to climate change.

• Knowledge: Develop a better understanding of the details of future climate change.

• Leadership: Raise public awareness of the challenges posed by climate change and the need to mitigate and adapt.