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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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TOPEX/El Niño Watch - Satellite shows Pacific Stabilizing, July 11, 1998
Title
TOPEX/El Niño Watch - Satellite shows Pacific Stabilizing, July 11, 1998
Title
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Original Caption Released with Image:
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height measurements taken by the U.S.-French TOPEX/Poseidon satellite. The image shows sea surface height relative to normal ocean conditions on July 11, 1998; sea surface height is an indicator of the heat content of the ocean. The purple area in the center of the image is a pulse of cold water moving across the equator which the satellite measures as a region of lower than normal sea level. This image shows that the rapid cooling of the central tropical Pacific has stabilized and this area of low sea level has stayed in about the same place since mid-June. The purple areas are about 18 centimeters (7 inches) below normal, creating a deficit in the heat supply to the surface waters. It is not certain yet, if this current cooling trend (shown in purple) will eventually evolve into a long-lasting La Niña situation. Remnants of the El Niño warm water pool, shown here in red and white, are still lingering to the north and south of the equator in the center of this image. The effects of El Niño can remain in the climate system for a long time and could still impact weather conditions around the world. The satellite's sea-surface height measurements have provided scientists with a detailed view of the 1997-98 El Niño because the TOPEX/Poseidon satellite measures the changing sea-surface height with unprecedented precision. In this image, the white areas show the sea surface is between 14 and 32 centimeters (6 to 13 inches) above normal; in the red areas, it's about 10 centimeters (4 inches) above normal. The green areas indicate normal conditions. The purple areas are 14 to 18 centimeters (6 to 7 inches) below normal and the blue areas are 5 to 13 centimeters (2 to 5 inches) below normal. The El Niño phenomenon is thought to be triggered when the steady westward blowing trade winds weaken and even reverse direction. This change in the winds allows a large mass of warm water (the red and white area) that is normally located near Australia to move eastward along the equator until it reaches the coast of South America. The displacement of so much warm water affects evaporation, where rain clouds form and, consequently, alters the typical atmospheric jet stream patterns around the world. A La Niña situation is essentially the opposite of an El Niño condition, where the trade winds are stronger than normal and the cold water that normally exists along the coast of South America extends to the central equatorial Pacific. A La Niña situation also changes global weather patterns, and is associated with less moisture in the air resulting in less rain along the coasts of North and South America. TOPEX/Poseidon will be able to track a potentially developing La Niña with the same accuracy.
Original_Caption_Rel eased_with_Image
height measurements taken by the U.S.-French TOPEX/Poseidon satellite. The image shows sea surface height relative to normal ocean conditions on July 11, 1998; sea surface height is an indicator of the heat content of the ocean. The purple area in the center of the image is a pulse of cold water moving across the equator which the satellite measures as a region of lower than normal sea level. This image shows that the rapid cooling of the central tropical Pacific has stabilized and this area of low sea level has stayed in about the same place since mid-June. The purple areas are about 18 centimeters (7 inches) below normal, creating a deficit in the heat supply to the surface waters. It is not certain yet, if this current cooling trend (shown in purple) will eventually evolve into a long-lasting La Niña situation. Remnants of the El Niño warm water pool, shown here in red and white, are still lingering to the north and south of the equator in the center of this image. The effects of El Niño can remain in the climate system for a long time and could still impact weather conditions around the world. The satellite's sea-surface height measurements have provided scientists with a detailed view of the 1997-98 El Niño because the TOPEX/Poseidon satellite measures the changing sea-surface height with unprecedented precision. In this image, the white areas show the sea surface is between 14 and 32 centimeters (6 to 13 inches) above normal; in the red areas, it's about 10 centimeters (4 inches) above normal. The green areas indicate normal conditions. The purple areas are 14 to 18 centimeters (6 to 7 inches) below normal and the blue areas are 5 to 13 centimeters (2 to 5 inches) below normal. The El Niño phenomenon is thought to be triggered when the steady westward blowing trade winds weaken and even reverse direction. This change in the winds allows a large mass of warm water (the red and white area) that is normally located near Australia to move eastward along the equator until it reaches the coast of South America. The displacement of so much warm water affects evaporation, where rain clouds form and, consequently, alters the typical atmospheric jet stream patterns around the world. A La Niña situation is essentially the opposite of an El Niño condition, where the trade winds are stronger than normal and the cold water that normally exists along the coast of South America extends to the central equatorial Pacific. A La Niña situation also changes global weather patterns, and is associated with less moisture in the air resulting in less rain along the coasts of North and South America. TOPEX/Poseidon will be able to track a potentially developing La Niña with the same accuracy.
Original Caption Released with Image
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Addition Date:
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1998-07-21
Addition_Date
1998-07-21
Addition Date
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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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TOPEX/Poseidon (Jason-1)
Mission
TOPEX/Poseidon (Jason-1)
Mission
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Spacecraft:
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TOPEX/Poseidon
Spacecraft
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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902 samples x 900 lines
Product_Size
902 samples x 900 lines
Product Size
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Primary Data Set:
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TOPEX/Poseidon Science and Data
Primary_Data_Set
TOPEX/Poseidon Science and Data
Primary Data Set
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Producer ID:
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P49964
MRPS89789
Producer_ID
P49964
MRPS89789
Producer ID
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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_where:
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Australia
facet_where
Australia
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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July 11, 1998
facet_when
July 11, 1998
facet_when
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facet_when_year:
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1998
facet_when_year
1998
facet_when_year
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Image #:
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PIA01461
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UID:
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SPD-PHOTJ-PIA01461
UID
SPD-PHOTJ-PIA01461
UID
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orignial url:
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orignial_url
orignial url
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