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Collection:
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NASA Planetary Photo Journal Collection
Collection
NASA Planetary Photo Journal Collection
Collection
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Title:
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A Mostly Quiet Pacific
Title
A Mostly Quiet Pacific
Title
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Original Caption Released with Image:
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Some climate forecast models indicate there is an above average chance that there could be a weak to borderline El Niño by the end of November 2003. However, the trade winds, blowing from east to west across the equatorial Pacific Ocean, remain strong. Thus, there remains some uncertainty among climate scientists as to whether the warm temperature anomaly will form again this year. The latest remote sensing data from NASA's Jason satellite show near normal conditions across the equatorial Pacific. There are currently no visible signs in sea surface height of an impending El Niño. This equatorial quiet contrasts with the Bering Sea, Gulf of Alaska and U.S. West Coast where lower-than-normal sea surface levels and cool ocean temperatures continue (indicated by blue and purple areas). The image above is a global map of sea surface height, accurate to within 30 millimeters. The image represents data collected and composited over a 10-day period, ending on Nov. 3, 2003. The height of the water relates to the temperature of the water. As the ocean warms, its level rises; and as it cools, its level falls. Yellow and red areas indicate where the waters are relatively warmer and have expanded above sea level, green indicates near normal sea level, and blue and purple areas show where the waters are relatively colder and the surface is lower than sea level. The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. The Jason satellite carries a dual-frequency radar altimeter. This instrument beam microwave pulses-at 13.6 and 5.3 Gigahertz, respectively-downwar d toward the Earth. To determine the ocean's height, the instrument precisely measures the time it takes for the microwave pulses to bounce off the surface and return to the spacecraft. This measure, multiplied by the speed of light, gives the range from the satellite to the ocean surface. (For more details, visit the Jason Website.)
Original_Caption_Rel eased_with_Image
Some climate forecast models indicate there is an above average chance that there could be a weak to borderline El Niño by the end of November 2003. However, the trade winds, blowing from east to west across the equatorial Pacific Ocean, remain strong. Thus, there remains some uncertainty among climate scientists as to whether the warm temperature anomaly will form again this year. The latest remote sensing data from NASA's Jason satellite show near normal conditions across the equatorial Pacific. There are currently no visible signs in sea surface height of an impending El Niño. This equatorial quiet contrasts with the Bering Sea, Gulf of Alaska and U.S. West Coast where lower-than-normal sea surface levels and cool ocean temperatures continue (indicated by blue and purple areas). The image above is a global map of sea surface height, accurate to within 30 millimeters. The image represents data collected and composited over a 10-day period, ending on Nov. 3, 2003. The height of the water relates to the temperature of the water. As the ocean warms, its level rises; and as it cools, its level falls. Yellow and red areas indicate where the waters are relatively warmer and have expanded above sea level, green indicates near normal sea level, and blue and purple areas show where the waters are relatively colder and the surface is lower than sea level. The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. The Jason satellite carries a dual-frequency radar altimeter. This instrument beam microwave pulses-at 13.6 and 5.3 Gigahertz, respectively-downwar d toward the Earth. To determine the ocean's height, the instrument precisely measures the time it takes for the microwave pulses to bounce off the surface and return to the spacecraft. This measure, multiplied by the speed of light, gives the range from the satellite to the ocean surface. (For more details, visit the Jason Website.) Original Caption Released with Image
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Image Credit:
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NASA/JPL Ocean Surface Topography Team
Image_Credit
NASA/JPL Ocean Surface Topography Team
Image Credit
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Produced By:
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JPL
Produced_By
JPL
Produced By
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Mission:
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Jason-1 (TOPEX/Poseidon)
Mission
Jason-1 (TOPEX/Poseidon)
Mission
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Spacecraft:
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Jason-1 (TOPEX/Poseidon)
Spacecraft
Jason-1 (TOPEX/Poseidon)
Spacecraft
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Target Name:
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Earth
Target_Name
Earth
Target Name
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Is a satellite of:
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Sol (our sun)
Is_a_satellite_of
Sol (our sun)
Is a satellite of
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Instrument:
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Altimeter
Instrument
Altimeter
Instrument
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Product Size:
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900 samples x 900 lines
Product_Size
900 samples x 900 lines
Product Size
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facet_what:
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Sun
facet_what
Sun
facet_what
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facet_what:
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Earth
facet_what
Earth
facet_what
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facet_what:
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TOPEX
facet_what
TOPEX
facet_what
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facet_what:
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Jason-1
facet_what
Jason-1
facet_what
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facet_what:
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Poseidon
facet_what
Poseidon
facet_what
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facet_what:
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TOPEX/Poseidon
facet_what
TOPEX/Poseidon
facet_what
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facet_what:
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Altimeter
facet_what
Altimeter
facet_what
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facet_what:
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Beam
facet_what
Beam
facet_what
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facet_what:
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Jason Satellite
facet_what
Jason Satellite
facet_what
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facet_where:
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Pacific Ocean
facet_where
Pacific Ocean
facet_where
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facet_where:
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Alaska
facet_where
Alaska
facet_where
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facet_where:
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Bering Sea
facet_where
Bering Sea
facet_where
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facet_where:
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Gulf of Alaska
facet_where
Gulf of Alaska
facet_where
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facet_where:
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Jet Propulsion Laboratory (JPL)
facet_where
Jet Propulsion Laboratory (JPL)
facet_where
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facet_when:
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November 2003
facet_when
November 2003
facet_when
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facet_when_year:
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2003
facet_when_year
2003
facet_when_year
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Image #:
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PIA04878
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UID:
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SPD-PHOTJ-PIA04878
UID
SPD-PHOTJ-PIA04878
UID
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orignial url:
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orignial_url
orignial url
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