Climate Change- the way the Earth has constantly evolved and changed temperature throughout history.

Slides:



Advertisements
Similar presentations
Global warming and CO2―Are we headed for global catastrophe in the coming century? Don J. Easterbrook.
Advertisements

14.3 Climatic Changes.
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.
Climate and Climate Change 17 January How and Why Does Climate Change? Climate changes over a broad range of time scales – Years, decades, centuries,
Fossils, Paleoclimate and Global Climate Change. Global Warming CO 2 levels in the atmosphere rising Average global temperature is rising Polar ice caps.
MET 112 Global Climate Change -
Arctic summers ice-free by 2013 predict scientists European heat waves kill 35, – the UK’s warmest year on record Rising sea levels threaten Pacific.
CLIMATE CHANGE Global Temperatures: Past, Present, and Future.
Lecture 3.2: What’s this “Greenhouse Effect” Thing anyway?
Lecture 12b Recent Warming. The Main Evidence The Global Temperature Record: today.
Essential Principles Challenge
Class #11: Wednesday July 21 Earth’s changing climate Chapter 16 1Class #11 Wednesday, July 21.
Unit 11 Notes: Climate Change
Climate Change Marge: We wouldn’t be in this predicament if you’d have paid the heat bill. Homer: Well, I thought Global Warming would go faster. That.
Climate and Climate Change
{ Natural Changes in Climate.  8.9 Long Term and Short Term Changes in Climate  8.10 Feedback Loops and Climate  8.11 Clues to Past Climates.
Chapter 4 Sections 3 and 4 Long Term Changes in Climate Global Changes in the Atmosphere.
 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 Change Global Warming Greenhouse Effect
CLIMATE CHANGE THE GREAT DEBATE Session 10. CLIMATE CHANGE? If we have learnt anything from this course, it is that climate is not constant It is, and.
Reviewing Climate Change Over Time Forcing Factors and Relevant Measurements.
Lecture 8 The Holocene and Recent Climate Change.
Chapter 14: Climate change The earth’s changing climate The earth’s changing climate Possible causes of climatic change Possible causes of climatic change.
Climate change – “science catfight” or not?. The Record Of Climate Change Proxy Data.
The past is the key to the future: Ice core isotope data, glacial fluctuations, decadal sea surface temperature changes, solar variations, and historic.
Sustainability and Globalization Global Warming. A global issue with regards to sustainability A world-wide warming of the Earth’s lower atmosphere.
DAISY WORLD, LIGHT/DARK DASIES EFFECT OF DASIES ON GLOBAL CLIMATE.
CLIMATE CHANGE THE GREAT DEBATE Session 7. SOLAR POWER The Sun is the primary driving force of climate and sits in the centre of the solar system that.
Global Energy Balance and the Greenhouse Effect What determines Earth’s surface temperature? What is the history of CO 2 on Earth? ultravioletinfrared.
Module 4 Changes in Climate. Global Warming? Climate change –The pattern(s) of variation in climate (temperature, precipitation) over various periods.
Lecture 31: Historical Climate: Volcanoes and Sunspots
14.3 – CLIMATIC CHANGES. Ice Age  Periods of extensive glacial coverage  Lots of ice sheets  Average global temperature decreased by about 5°C  Most.
Lecture 15 Defining climate, climate controls Climate classification
Global Climate Change A long term perspective. Global Warming CO 2 levels in the atmosphere rising Average global temperature is rising Polar ice caps.
Evidence of Global Warming and Consequences
Climate and Climate Change Chapter 21
Abrupt Climate Change. Review of last lecture Large spread in projected temperature change comes from uncertainties in climate feedbacks Main climate.
Edexcel AS Geography Unit 1 – Global Challenges (6GE01) World at Risk Climate change and its causes – Part B.
Chapter 13: The Earth’s Changing Climate Climate change Climate change Possible causes of climatic change Possible causes of climatic change Global warming.
Causes of Climate Change Think: What is climate change? (key words you have heard on the news, important impacts, etc) Global Climate Change
WHAT IS IT AND WHAT ARE SCIENTISTS DOING TO GATHER INFORMATION ABOUT IT? Climate Change.
 On a climograph, what data are represented with bars? ◦ What data are represented with a line graph?  How can you determine the climate classification.
Natural Causes of Climate Change. Volcanic Eruptions Eject tons of SO 2 and ash into the atmosphere. These substance reflect solar radiation back into.
Starter 2/19/15  Think about what the term “climate” means to you. List words that come to mind when you think of climate!!!
Long-Term Changes in Climate
Causes of Global Warming. “Over the last few decades there’s been much more evidence for the human influence on climate…. We’ve reached the point where.
© 2014 Pearson Education, Inc. The Oceans and Climate Change Chapter 1 Clickers Essentials of Oceanography Eleventh Edition Alan P. Trujillo Harold V.
Natural Causes of climate change. Volcanic eruptions Volcanic eruptions eject tons of SO 2 and ash into the atmosphere. These substance reflect solar.
Climate. Weather vs. Climate Weather – the condition of Earth’s atmosphere at a particular time and place. – Short-term: Hours and days – Localized: Town,
What makes a good argument? Make a list of things you think contribute to a convincing argument.
Climate Change – is it really happening? Kathy Maskell Walker Institute for Climate System Research, University of Reading.
Unit 3 Notes Part 5: Climate Change. What are natural causes that could result in global climate change? Plate tectonics – when the continents move they.
© 2014 Pearson Education, Inc. Chapter 16 The Oceans and Climate Change.
To recap Give 2 examples of research methods that show long term historical climate change? How reliable are these? Give 2 ways of measuring medium term.
Natural Causes of climate change
Climate Change Climate – The average year after year pattern of temperature, precipitation, winds and clouds in an area. Climates are classified mainly.
Earth’s Climate System
14.3 Climatic Changes.
Natural Causes of Climate Change
Chapter 14: Climate Change
Natural & anthropogenic causes
DO NOW Pick up notes and Review #25..
Climate Changes due to Natural Processes
Long-Term Changes in Climate
Long-Term Changes in Climate
AOSC 200 Lesson 23.
Climate Changes due to Natural Processes
PAPER 1: Living with the physical environment
Natural Changes in Climate
Climate Change.
Presentation transcript:

Climate Change- the way the Earth has constantly evolved and changed temperature throughout history

Homo Sapiens Industrialisation

The sceptic argument... Earth's climate has changed long before we were pouring CO2 into the atmosphere. Europe was far warmer in the Middle Ages. During the 17th and 18th century, it was much colder, prompting the ‘The Little Ice Age’, when the Thames was frozen over months at a time. Further back, there were times when the Earth was several degrees hotter than current temperatures. Warming of several degrees often took only centuries or decades. Discuss with a partner why some people may be skeptical about climate change. Who may these people be?

Background The 16th century is the first period for which we have a reliable history of climate and weather. Private diaries, ships' logs, accounts of military campaigns, and similar sources give descriptions of wind direction, wind speed, cloud formations, and other weather indicators. Precisely dated annals, chronicles, audited accounts, agricultural records, tax ledgers, and other archival material provide indirect information, particularly on extreme weather events, such as droughts, floods, or unusual cold. Additional evidence is available from glacial moraines, lake and ocean sediments, pollen strata, deposits of insects, tree rings, coral structure, radiometric analysis of ice cores, archaeological sites, and many other sources. All this information can be combined to reconstruct past climates

Natural causes for climate change

Solar activity Solar variations have been the major driver of climate change over the past 10,000 years. When sunspot activity was low during the Maunder Minimum in the 1600's or the Dalton Minimum in the 1800's, the earth went through 'Little Ice Ages'. Similarly, solar activity was higher during the Medieval Warm Period. However, the correlation between solar activity and global temperatures ended around At that point, temperatures started rising while solar activity stayed level. This led a Finnish and German scientists to conclude "during these last 30 years the solar total irradiance, solar UV irradiance and cosmic ray flux has not shown any significant secular trend, so that at least this most recent warming episode must have another source

Caption for Image Four: The Sun shows signs of variability, such as its eleven-year sunspot cycle. In that time, it goes from a minimum (seen here in 1996) to a maximum (2000) period of activity that affects us everyday. When particularly active, solar storms can spew tons of radiation to Earth in the form of Coronal Mass Ejections (CMEs) that can affect power grids, spacecraft, and communication systems. SUPER: NASA / ESA

Changes in solar output

Milankovitch cycles Earth's climate undergoes 120,000 year cycles of ice ages broken by short warm periods called interglacials. The cycle is driven by Milankovitch cycles. Long term changes in the Earth's orbit trigger an initial warming which warms the oceans and melts ice sheets - this releases CO2. The extra CO2 in the atmosphere causes further warming leading to interglacials ending the ice ages. For the past 12,000 years, we've been in an interglacial. The current trend of the Milankovitch cycle is a gradual cooling down towards an ice age.

Changes in earths orbit

Volcanoes Volcanic eruptions spew sulphate aerosols into the atmosphere which has a cooling effect on global temperatures. These aerosols reflect incoming sunlight, causing a 'global dimming' effect. Usually, the cooling effect lasts several years until the aerosols are washed out of the atmosphere. In the case of large eruptions or a succession of eruptions such as in the early 1800's, the cooling effect can last several decades. Strong volcanic activity exacerbated the Little Ice Age in the 1800's. Observational and modelling studies (e.g. Kelly & Sear, 1984; Sear et al., 1987) of the likely effect of recent volcanic eruptions suggest that an individual eruption may cause a global cooling of up to 0.3°C, with the effects lasting 1 to 2 years. Such a cooling event has been observed in the global temperature record in the aftermath of the eruption of Mount Pinatubo in June The climate forcing associated with individual eruptions is, however, relatively short-lived compared to the time needed to influence the heat storage of the oceans (Henderson-Sellers & Robinson, 1986). The temperature anomaly due to a single volcanic event is thus unlikely to persist or lead, through feedback effects, to significant long-term climatic changes.

Catastrophic events-e.g. volcanic eruptions

Sample question

Mark scheme