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Modern Climate Change Darryn Waugh [email protected] OES Summer Course, July 2015
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Page 1: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Modern Climate Change

Darryn Waugh

[email protected]

OES Summer Course, July 2015

Page 2: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

IS THE EARTH’S TEMPERATURE CHANGING?

Focus on last 160 yrs

Page 3: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Climate over last 160 Years

Surface measurements show clear warming over last 100 yrs. Last decade warmest on record.

Annual average Temperature (relative to 1961-1990)

Page 4: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Climate over last 160 Years

Page 5: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Past Climate: Last 2000 years

Large uncertainty in temperature before 1850s, but all reconstructions show that global temperatures over last 30-40 years have not occurred in at least 2000 years.

Page 6: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Spatial Variations in Temperature Trends

Although global warming has occurred, this does not mean warming everywhere. More rapid warming over land than oceans.

[IPCC AR5]

Page 7: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

WHAT ARE OTHER CHANGES IN THE CLIMATE SYSTEM?

Page 8: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Ocean Heat Content & Sea Level

[IPCC AR5]

Page 9: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Arctic Sea Ice

Page 10: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

[IPCC AR5]

Land Surface Temp.

Sea Surface Temp.

Marine Air Temp.

Sea Level

Arctic Sea Ice

NH Snow Cover

Glacier Mass Balance

Specific Humidity

Ocean Heat Content

Tropo-spheric Temp.

Page 11: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Reading Material

Homework

[IPCC AR5]

Observed Changes in Climate System

Page 12: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Positive Proof

Page 13: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

WHAT ARE THE CAUSES OF MODERN CLIMATE CHANGE?

What has caused for the observed warming over the last 160 yrs?

Page 14: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

WHAT HAS CAUSED THE RECENT CHANGE IN EARTH’S TEMPERATURE?

The suspects:– Orbital variations– Volcanoes– Solar Irradiance– Internal variability– Greenhouse gases

Page 15: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

The suspects:– Orbital variations– Volcanoes– Solar– Internal variability– Greenhouse gases

For last 50 yrsN time scale too long (>10,000 yrs)N no sustained forcing (2-3 yrs)N no trend since 1960s N inconsistent with last 2000 yr record

Y time scale correct + consistent with theory and measurements.

WHAT HAS CAUSED THIS CHANGE IN EARTH’S TEMPERATURE?

Page 16: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Surface Temperature and Solar Variations

No trend in solar irradiance in recent decades => Changes in solar irradiance can not explain increase in surface temperature over this period.

Page 17: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

IPCC, 2007

Greenhouse Effect

Page 18: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Absorption by Gases

Page 19: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Atmospheric CO2: 1958 to present

Surface CO2 measurements show long-term increase + annual cycle

Mauna Loa

South Pole

Page 20: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Atmospheric CO2: 1000 to present

Page 21: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Greenhouse Gases (GHGs)

Concentrations of CO2, N2O, CH4 (“Greenhouse Gases”) have increased dramatically over last 150 yrs.

Page 22: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Temperature and CO2

20001000

1st Oil Well

Page 23: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Attribution

Need to also consider changes in aerosols, clouds and land surface (as well as solar, volcanic eruptions, etc.) for a quantitative understanding of cause of warming.

Increases in GHGs has been major contributor to warming.

Page 24: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

WHAT MIGHT HAPPEN IN THE FUTURE?

To make projections of the future climate need

1. Numerical models to integrate together different components and processes, and

2. Projections of future emissions of greenhouse gases (and changes in land use), which depends on human behavior and activities.

Page 25: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Climate Models

Page 26: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Predicting Future Emissions

Future emissions of greenhouse gases (and changes in land use) will depend on several on different factors. E.g.

• Global Population trends

• World Economic Growth

• Source of Energy

• Technological Trends

• Policies

• Historical events (wars, political transitions).

All above are affected by human behavior and activities.

Page 27: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

CO2 Emission Scenarios

A1B - balance between fossil and non-fossil fuels.

A1F1 - fossil fuel intensive.

A1T - large shift to non-fossil fuel.

B1 - sustainable development

A2 - heterogeneous would .

[IPCC 2001] Projections since 2001

Page 28: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Temperature Projections: 2005-2100

High Emissions

Low Emissions

Page 29: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Temperature Changes: Spatial variations

Warming is largest in NH high latitudes (ice feedback) and larger over land than oceans (heat capacity).

Minimum over North Atlantic Ocean and Southern Ocean

High EmissionsLow Emissions

Page 30: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Sea Level Rise

High Emissions

Low Emissions

Page 31: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Sea Ice Predictions

• All models predict continued retreat of Arctic sea ice. • Some predict complete ice free summers by end of the century.

Page 32: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Rainfall

Less rain in dry regions - DroughtsMore rain in wet regions - Floods.

High EmissionsLow Emissions

Page 33: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Heat Stress

Page 34: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

“Global Climate Change Impacts in the US”

Report from US Global Change Research Program

http://www.globalchange.gov

Impacts separated by Regions and Sectors

Page 35: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Impacts of Climate Change

Page 36: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

“What’s the worst that could happen?” [A rational response to climate change debate]

Greg Carven

http://www.youtube.com/watch?v=zORv8wwiadQ

http://manpollo.org/education/videos/how_it_all_ends/how_it_all_ends.html

Page 37: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Areas of Response

Geoengineering

• Mitigation - reduce the emissions of GHGs that cause climate change.• Geoengineering - manipulate the climate system to offset climate

effects of increased GHGs.• Adaptation - adjust human society to changing climate to reduce

resulting harms.

Page 38: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.
Page 39: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

Stabilization Wedges

Page 40: Modern Climate Change Darryn Waugh waugh@jhu.edu OES Summer Course, July 2015.

TAKE-HOME MESSAGES

Restatement of IPCC (2013) conclusions:

• We know that the climate is warming.

• We’re very sure humans are to blame.

• The future is hard to predict, but it’s certainly possible that

“business as usual” will lead to a catastrophic warming.

Contact: Darryn Waugh

[email protected]

410-516-8344.