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Earth ScienceEarth Science
Presentation toPresentation to
American Astronautical SocietyAmerican Astronautical Society
Conference on Astronauts and Robots:
Partners in Space Science and Exploration
May 13, 2015May 13, 2015
Randall R. FriedlRandall R. Friedl
Jet Propulsion Laboratory
California Institute of Technology
"The Earth is a very small stage in a
vast cosmic arena. … Our
posturings, our imagined self-
importance, the delusion that we
have some privileged position in the
Universe, are challenged by this
point of pale light.“
-- Carl Sagan
From "Pale Blue Dot: A Vision of
the Human Future in Space,"
Random House, 1994
View from Voyager
View from Mars
Space observations provide a new
perspective on Earth
Jet Propulsion Laboratory
California Institute of Technology
Space observations reveal an inter-connected
Earth system
MISR - aerosols
MLS – ozone layer
TES – trace gas
AIRS – atmospheric temperature
CLOUDSAT – water content
JASON – sea surface height
QUIKSCAT – wind
GRACE – gravity
Aquarius - sea surface salinity
Jet Propulsion Laboratory
California Institute of TechnologySpace observations track Earth
transformations
Defense Meteorological Satellite Program (DMSP)
Operational Linescan System (OLS)
Jet Propulsion Laboratory
California Institute of Technology
At many spatial scales
1988
Pearl River Delta, China: Landsat false
color image
Chandler Arizona: Landsat True color
image
From NASA/USGS
Jet Propulsion Laboratory
California Institute of Technology
Sea Surface Temperature
(left) and Rainfall (Right)
anomalies in the Eastern
Pacific
From NASA’s Earth
Observatory based on
AVHRR and blended rainfall
data from multiple satellites
1997
2007
Example 1: Understanding El Nino,
La Nina, and Rainfall Patterns
Jet Propulsion Laboratory
California Institute of TechnologyExample 2: Projecting sea level rise
Satellite
Record
From TOPEX/Poseidon
And Jason series
3.0 m0.3 m Average Global Sea Level Rise
Over the Next 10 Years
100
50
0
%Probability
Greenland ice
mass loss, from
NOAA Arctic
Report Card
Jet Propulsion Laboratory
California Institute of Technology
Example 3: Understanding Arctic
sea ice inter-annual processes and
longer-term trends
2002
2008 2015
From NASA Earth Observatory
Based on SSMI/DMSP data
Jet Propulsion Laboratory
California Institute of Technology
1979 1990
2001 2013
From NASA Earth Observatory, based on TOMS/OMI data
Example 4: Understanding Antarctic ozone
inter-annual processes and longer-term
trends
Example 5: Understanding ground waterExample 5: Understanding ground water
storage changesstorage changes
Landerer, JPL
Jet Propulsion Laboratory
California Institute of Technology
GW
SW
Groundwater depletion during drought
threatens future water security of the
Colorado River Basin,
(from Castle et al., 2014)
Surface and ground water storage
anomalies from GRACE data
Jet Propulsion Laboratory
California Institute of Technology
Example 6: Characterizing Fault Slip and Crustal
Motion
• Central creeping segment (AA’ to DD’): nonuniform creeping at shallow depth (~0-6km) and partially locked at upper
crustal level (~6-10km)
• Parkfield segment (EE’ to GG’): creeping at 0-4 km and locked at variable depth range
• Increased coupling towards Parkfield and fully locked in 1857 EQ rupture area (HH’ and beyond)
(Liu, et al, 2011)

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Astronauts and Robots 2015: Randall Friedl, JPL

  • 1. Earth ScienceEarth Science Presentation toPresentation to American Astronautical SocietyAmerican Astronautical Society Conference on Astronauts and Robots: Partners in Space Science and Exploration May 13, 2015May 13, 2015 Randall R. FriedlRandall R. Friedl
  • 2. Jet Propulsion Laboratory California Institute of Technology "The Earth is a very small stage in a vast cosmic arena. … Our posturings, our imagined self- importance, the delusion that we have some privileged position in the Universe, are challenged by this point of pale light.“ -- Carl Sagan From "Pale Blue Dot: A Vision of the Human Future in Space," Random House, 1994 View from Voyager View from Mars Space observations provide a new perspective on Earth
  • 3. Jet Propulsion Laboratory California Institute of Technology Space observations reveal an inter-connected Earth system MISR - aerosols MLS – ozone layer TES – trace gas AIRS – atmospheric temperature CLOUDSAT – water content JASON – sea surface height QUIKSCAT – wind GRACE – gravity Aquarius - sea surface salinity
  • 4. Jet Propulsion Laboratory California Institute of TechnologySpace observations track Earth transformations Defense Meteorological Satellite Program (DMSP) Operational Linescan System (OLS)
  • 5. Jet Propulsion Laboratory California Institute of Technology At many spatial scales 1988 Pearl River Delta, China: Landsat false color image Chandler Arizona: Landsat True color image From NASA/USGS
  • 6. Jet Propulsion Laboratory California Institute of Technology Sea Surface Temperature (left) and Rainfall (Right) anomalies in the Eastern Pacific From NASA’s Earth Observatory based on AVHRR and blended rainfall data from multiple satellites 1997 2007 Example 1: Understanding El Nino, La Nina, and Rainfall Patterns
  • 7. Jet Propulsion Laboratory California Institute of TechnologyExample 2: Projecting sea level rise Satellite Record From TOPEX/Poseidon And Jason series 3.0 m0.3 m Average Global Sea Level Rise Over the Next 10 Years 100 50 0 %Probability Greenland ice mass loss, from NOAA Arctic Report Card
  • 8. Jet Propulsion Laboratory California Institute of Technology Example 3: Understanding Arctic sea ice inter-annual processes and longer-term trends 2002 2008 2015 From NASA Earth Observatory Based on SSMI/DMSP data
  • 9. Jet Propulsion Laboratory California Institute of Technology 1979 1990 2001 2013 From NASA Earth Observatory, based on TOMS/OMI data Example 4: Understanding Antarctic ozone inter-annual processes and longer-term trends
  • 10. Example 5: Understanding ground waterExample 5: Understanding ground water storage changesstorage changes Landerer, JPL Jet Propulsion Laboratory California Institute of Technology GW SW Groundwater depletion during drought threatens future water security of the Colorado River Basin, (from Castle et al., 2014) Surface and ground water storage anomalies from GRACE data
  • 11. Jet Propulsion Laboratory California Institute of Technology Example 6: Characterizing Fault Slip and Crustal Motion • Central creeping segment (AA’ to DD’): nonuniform creeping at shallow depth (~0-6km) and partially locked at upper crustal level (~6-10km) • Parkfield segment (EE’ to GG’): creeping at 0-4 km and locked at variable depth range • Increased coupling towards Parkfield and fully locked in 1857 EQ rupture area (HH’ and beyond) (Liu, et al, 2011)

Notas do Editor

  1. GRACE measures all the water storage changes on land to estimate groundwater, the snow, surface water and soil moisture changes must be subtracted Result: even after official drought ended in 2010, GRACE detects that Central Valley groundwater still remains below pre-drought levels