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Global Warming

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... Warming. Problem. Global warming affects us all. The Earth has warmed up ... Man-made emissions of greenhouse gases have increased (burning of fossil fuels ... – PowerPoint PPT presentation

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Title: Global Warming


1
Global Warming
2
Problem
  • Global warming affects us all.
  • The Earth has warmed up by about 0.6C in the
    last 100 years.
  • Man-made emissions of greenhouse gases have
    increased (burning of fossil fuels and
    deforestation)

3
20 years ago, what was the scenario?
  • CO2 measurements (Mauna Loa)
  • Ice core measurements (Only back 100.000 yrs)
    based on ice deposition
  • Scattered sea surface temperature measurements
  • Rough estimates of ice thickness in the poles

4
New Techniques
  • Satellite images

(Larsen B Ice Shelf)
From NASA MODIS instrument, 2002
5
New Techniques
  • Ice core analysis
  • Methane
  • CO2
  • deuterium
  • dust flux
  • Gas Age
  • Ice Age
  • temperature difference from present

NASA
6
New Techniques
  • Environmental gas estimates-more accurate and
    long-term
  • Automated SST measurements throughout all the
    oceans

7
New Techniques
  • Better understanding of ocean circulation Global
    Conveyor Belt, and of glaciations

From Gateways to Glaciation, ODP
8
New Techniques
  • Access to deep ocean sediments to understanding
    how Earth's climate could change

From Ocean Drilling program site
9
New Techniques
  • Paleomagnetism

From Ocean Drilling program site
10
Data availability and support
  • Currently one of the most debated fields
    several researchers involved
  • NOAA/NASA data online
  • DLESE and other servers available for educational
    research

11
El Niño Southern Oscillation (ENSO)
12
Problem
  • It is a global phenomenon that impacts us all,
    one way or the other
  • Represents changes in the circulation of the
    Tropical Pacific and the global atmosphere
    (changes in atmospheric pressure over the Pacific
    and weak trade winds)
  • Is associated with ecological and economic losses
    around the globe

13
How did we know about ENSO?
  • Discrete data from fishermen
  • Temperature and pressure anomalies in the Pacific
    measured in few stations
  • Droughts, excessive rain and other isolated
    phenomena that were not directly linked to ENSO

14
New Tech
  • General Circulation Models

Source NOAA El Niño resource web page
15
New Tech
  • Pressure anomaly measurements at key stations in
    the Pacific (Darwin, Australia Tahiti
    Southern Oscillation Index)

16
New Tech
  • Satellite altimetry and temperature measurements,
    real-time.

Source NOAA El Niño resource web page
17
New Tech
  • Coral and sediment paleoclimatology El Niño has
    waxed and waned over millennia.

Source NOAA Paleoclimatology Program/Department
of Commerce
18
New Tech
  • Well defined pattern and intensity of La Niña/El
    Niño

Source NOAA El Niño resource web page
19
New Tech
  • TAO buoy array (NOAA)

Source TAO resource web page
20
New Tech
  • Drifting buoy data (NOAA)
  • Gliders
  • Automated Sea Level and rainfall gauges

Source https//www.navo.navy.mil
21
New Tech
  • Shipboard measurements (NOAA ship KA'IMIMOANA
    (Ocean Seeker)

Source TAO resource web page
22
Data availability and support
  • TOGA research program
  • NOAA El Niño resource web page daily updated
    (http//www.pmel.noaa.gov/tao/elnino/el-nino-story
    .html)
  • Large amount of web resources (best University or
    government resources) Other sources are
    educational (e.g. DLESE, NOAA)
  • Several researchers at Universities just ask!
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