Volcanoes and Climate. The Earth’s Energy (Radiation) Budget.

Slides:



Advertisements
Similar presentations
Greenhouse Effect As sunlight enters the Earth’s atmosphere, some of the radiation from the sun is reflected back into outer space But, some of that radiation.
Advertisements

Heat Budget and Climate Change. Heat Budget is the result of a balance between energy received (insolation and Earth’s Interior) and energy lost (terrestrial.
Atmosphere & Climate Change
Impacts of volcanism on climate. Natural events that can trigger global climate changes include: (1) known astronomical variations in the orbital elements.
Climatology Climatology is the study of Earth’s climate and the factors that affect past, present, and future climatic changes. Climate describes the long-term.
8-1 Notes - Geologic Time and Mass Extinctions
1 Volcanoes. 2 Different Volcanic Settings 3 Types of Eruptions Eruptions will generally be of two types: Quiet (Rift) eruptions Explosive (Subduction)
Our atmosphere is perilously thin. Yet it provides important solar protection as well as oxygen.
Factors that Influence Climate
Class #11: Wednesday July 21 Earth’s changing climate Chapter 16 1Class #11 Wednesday, July 21.
CHAPTER 5. * Weather is daily changes in temp and precipitation. * CLIMATE is the average year to year conditions.
Prentice Hall EARTH SCIENCE
Climate Change UNIT 3 Chapter 7: Earth’s Climate System
Unit 1 – Climate Change
 The difference between weather and climate is a measure of time. Weather is what conditions of the atmosphere are over a short period of time, and climate.
Climate.
TOPIC 6: INSOLATION AND THE SEASONS
What is an Ice Age ? Ice ages are times when large areas of the earths surface are covered with ice sheets The term is used to describe time periods when.
1 Volcanoes Volcano Cam. 2 Different Volcanic Settings.
Plate Tectonic and Ocean Bathymetry. Effects of Volcanic eruptions on the solar incoming radiation Agung 1963 Pinatubo 1991 Chichón 1982 Pinatubo.
Climate change – “science catfight” or not?. The Record Of Climate Change Proxy Data.
Chapter 13: Atmosphere & Climate Change
Atmosphere and Climate ChangeSection 1 Climate average weather conditions in an area over a long period of time. determined by factors that include: latitude,
Atmosphere and Climate ChangeSection 1 Section 1: Climate and Climate Change Preview Bellringer Objectives Climate Latitude Atmospheric Circulation Global.
Objectives Explain the difference between weather and climate.
21.3 Climate Change. Natural Processes That Change Climate Volcanic eruptions The presence of volcanic ash, dust, & aerosols in the air increases the.
Volcanoes Chapter 15 Section 2.
Climates.
Taylor Delph James Cannariato Kayla Abrott Abby Grove Ashley George.
WORLD GEOGRAPHY December 9, Today Unit 10 (Human Environment)
DAISY WORLD, LIGHT/DARK DASIES EFFECT OF DASIES ON GLOBAL CLIMATE.
Lecture 31: Historical Climate: Volcanoes and Sunspots
Major Factors affecting climate
Climate and Climate Change Environmental Science Spring 2011.
The sun is the primary source of Energy to Earth’s climate system.
Lecture 15 Defining climate, climate controls Climate classification
Bellringer. Climate Climate is the average weather conditions in an area over a long period of time. – determined by a variety of factors including: latitude,
Day one Chapter 13 Atmosphere and Climate Change
UNIT 3 Climate Change 1.
 What is your view on climate change? Write down either: What you believe about climate change What you have heard someone say about climate change 
Geologic Time and Mass Extinctions
Climate -Climate is the average weather conditions in an area over a long period of time. -Climate is determined by a variety of factors that include latitude,
Mt Everest You should have created a table of impacts. Walk around the class and add to your table.
Near Extinction Of Humans.
Climates can change suddenly or slowly.  ICE AGE: Period in which huge sheets of ice spread out beyond the polar regions.  El NINO: A disturbance of.
The Atmosphere A thin fragile shell of gases that provides all our weather and allows life on earth.
Unit 4: Climate Change Earth’s Climate System. Introduction Atmosphere: layer of gases that surrounds a planet or moon Without the atmosphere, days would.
DAY ONE Chapter 13 Atmosphere and Climate Change Section 1: Climate and Climate Change.
Ch. 13 Section 1. Objective Compare and contrast weather and climate. List and describe factors that influence them and analyze their impact.
1. Climate Climate is the average weather conditions in an area over a long period of time. Climate is determined by a variety of factors that include.
Section 1: Climate Preview Classroom Catalyst Objectives Climate
Climate and Climate Change
Volcanoes and Climate.
Natural Causes of Climate Change
Day one Chapter 13 Atmosphere and Climate Change
Climate and Climate Change
Bellringer.
Volcanoes and Climate.
Pinatubo – a case study.
The Atmosphere.
Volcanoes Key Question: How are volcanoes hazardous to human populations and what controls risk? Key Words Risk and Hazard Primary and Secondary Effects.
Pinatubo – a case study.
Day one Chapter 13 Atmosphere and Climate Change
Dark Skies: Volcanic Contribution to Climate Change
Day one Chapter 13 Atmosphere and Climate Change
Section 1: Climate Preview Classroom Catalyst Objectives Climate
Climate.
Climate Change.
ENVIRONMENTAL SCIENCE
Presentation transcript:

Volcanoes and Climate

The Earth’s Energy (Radiation) Budget

Pinatubo 1963 Agung 1982 El Chichon Santa Maria 1902

Atmospheric Stability Many things can cause air to rise As it rises, the pressure falls and the air cools If the air is then warmer than the surrounding air, it carries on rising – unstable. If the air is colder than the surrounding air, it sinks back to where is came from – stable. The stratosphere is always very stable – but explosive volcanic eruptions can blast material up into the stratosphere. Once in the stratosphere, the stability means that the volcanic materials tends to stay there for several years.

Explosive volcanoes and latitude Stratospheric circulation Tropospheric circulation

For maximum effect a volcano should be… -Explosive -Low latitude -Effects are greater over land than over sea -Northern hemisphere summer season -Lots of Sulphur dioxide emitted.

Volcanic forcing of climate over the past 1500 years: An improved ice core- based index for climate models 2008, Chaochao Gao, Alan Robock, and Caspar Ammann

Effusive or small volcanoes - e.g. Bárðabunga, Explosive volcanoes Super volcanoes or intense volcanic activity -Snowball Earth (pre-Cambrian) -Super volcanoes - any volcano capable of producing a volcanic eruption with an ejecta mass greater than kg -Toba, Sumatra (74,000 years ago), preceded major glaciation -Yellowstone (640,000 years ago), 5°C global cooling

Laki & Grímsvötn, Lasted for eight months during 1783 to 1784, and produced one of the largest basaltic lava flows in historic times The release of sulphur gases during fountaining produced an acid haze (aerosol) which spread widely and had a considerable environmental, and possibly climatic, impact on the Northern Hemisphere. Troposphere, not stratosphere Fire-fountains of magma reached 1.4km, ash reached 9-13km The quantity of SO 2 released was comparable to the total annual present-day anthropogenic input to the atmosphere

Laki & Grímsvötn, During the explosive phases, the atmosphere over Iceland became loaded with fine ash and sulphuric acid droplets. Grass growth was stunted, 50% of grazing livestock died and 22% of Icelanders died. Haze or dry fog was reported over much of the Northern Hemisphere, blood red sunsets – affected vegetation, animals and people Summer of 1783 was warm, was colder than usual, but was it due to the volcano? Linked to famine and plague in middle east, virtual dying out of Inuit in NW Alaska Did the aerosol reach the stratosphere? Food poverty was a major factor in the build-up to the French revolution of 1789

Eyjafjallajökull, 2010

Volcanoes and Climate Change? Climate Change Less Ice Less Pressure More magma generation c.org/2015/11/icelands- volcanic-activity-to- increase-from-climate- change/