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Myneni L30: Projections of Future Climate Change Apr-20-07 (1 of 10). Natural Environments: The Atmosphere GE 101 – Spring 2007 Boston University. Further Reading: Detailed Notes Posted on Class Web Sites. Outline. global climate models the next two decades 21st century projections

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slide1

Myneni

L30: Projections of Future Climate Change

Apr-20-07

(1 of 10)

Natural Environments: The Atmosphere

GE 101 – Spring 2007

Boston University

Further Reading: Detailed Notes Posted on Class Web Sites

Outline

  • global climate models
  • the next two decades
  • 21st century projections
  • - summary of changes from IPCC 2007
slide2

Myneni

L30: Projections of Future Climate Change

Apr-20-07

(2 of 10)

Natural Environments: The Atmosphere

GE 101 – Spring 2007

Boston University

Introduction

The purpose of this chapter is to assess and quantify projections of possible future climate

change from climate models.

The Climate System

slide3

Myneni

L30: Projections of Future Climate Change

Apr-20-07

(3 of 10)

Natural Environments: The Atmosphere

GE 101 – Spring 2007

Boston University

Global Climate Models

Global climate models (GCMs) include as central components atmospheric and ocean general circulation models, as well as representation of land surface processes, and sea-ice.

slide4

Myneni

L30: Projections of Future Climate Change

Apr-20-07

(4 of 10)

Natural Environments: The Atmosphere

GE 101 – Spring 2007

Boston University

The Next 2 Decades

For the next two decades a warming of about 0.2°C per decade is

projected for a range of emission scenarios.

Even if the concentrations of all greenhouse gases and aerosols had

been kept constant at year 2000 levels, a further warming of about

0.1°C per decade would be expected.

slide5

Myneni

L30: Projections of Future Climate Change

Apr-20-07

(5 of 10)

Natural Environments: The Atmosphere

GE 101 – Spring 2007

Boston University

21st Century- Global Average Temperature

B1: Low emissions, A2: High Emissions

slide6

Myneni

L30: Projections of Future Climate Change

Apr-20-07

(6 of 10)

Natural Environments: The Atmosphere

GE 101 – Spring 2007

Boston University

21st Century - Temp and Sea Level Rise

slide7

Myneni

L30: Projections of Future Climate Change

Apr-20-07

(7 of 10)

Natural Environments: The Atmosphere

GE 101 – Spring 2007

Boston University

21st Century - Pattern of Warming

Projected surface temperature changes for the early and late 21st

century relative to the period 1980– 1999

slide8

Myneni

L30: Projections of Future Climate Change

Apr-20-07

(8 of 10)

Natural Environments: The Atmosphere

GE 101 – Spring 2007

Boston University

21st Century - Precip Patterns

Relative changes in precipitation (in percent) for the period 2090–2099,

relative to 1980–1999. Values are multi-model averages based on the

medium emission scenario for December to February (left) and June to

August (right).

slide9

Myneni

L30: Projections of Future Climate Change

Apr-20-07

(9 of 10)

Natural Environments: The Atmosphere

GE 101 – Spring 2007

Boston University

21st Century - IPCC 2007 Projections-1

Continued greenhouse gas emissions at or above current rates would

cause further warming and induce many changes in the global climate

system during the 21st century that would very likely be larger than

those observed during the 20th century.

Warming is expected to be greatest over land and at most high northern

latitudes, and least over the Southern Ocean and parts of the North

Atlantic ocean.

Snow cover is projected to contract. Sea ice is projected to shrink in

both the Arctic and Antarctic under all emission scenarios. In some

projections, Arctic late-summer sea ice disappears almost entirely by

the latter part of the 21st century.

slide10

Myneni

L30: Projections of Future Climate Change

Apr-20-07

(10 of 10)

Natural Environments: The Atmosphere

GE 101 – Spring 2007

Boston University

21st Century - IPCC 2007 Projections-2

Increases in the amount of precipitation are very likely in high

latitudes, while decreases are likely in most subtropical land regions

(by as much as about 20%), continuing observed patterns in recent

trends.

It is very likely that hot extremes, heat waves, and heavy precipitation

events will continue to become more frequent.

Based on a range of models, it is likely that future tropical cyclones

(typhoons and hurricanes) will become more intense, with larger peak

wind speeds and more heavy precipitation associated with ongoing

increases of tropical SSTs.