The international Sentinel-6 Michael Freilich sea
level satellite observed a swell of warm water, called a Kelvin wave, moving
eastward in the equatorial Pacific Ocean, arriving off the South American coast
in May. Warm Kelvin waves often precede El Niño events.
NASA/JPL-Caltech
Sea level data from a satellite launched by NASA and European partners
shows that a swell of warm water hundreds of miles wide has arrived in the
Pacific Ocean off the coast of South America, a sign that El Niño will likely
emerge later in the year. Because water expands as it warms, a rise in
elevation of an area of the ocean indicates increasing ocean temperatures.
El Niños can cause heavy
precipitation in some regions and deficits in others, influencing daily life
and commerce around the world.
Launched in 2020 by NASA and led by
ESA (European Space Agency) for the E.U. Copernicus Programme, the Sentinel-6 Michael Freilich satellite measures and maps water height for the
entire ocean every 10 days, down to fractions of an inch. In the case of El
Niño, the satellite tracks what are called warm Kelvin waves.
These waves typically form after
brief periods when winds over the far western equatorial Pacific Ocean shift
from prevailing easterlies — moving from east to west — to westerlies. That
effect, combined with a general weakening of easterly winds along the equator,
causes water in the tropics of the western Pacific to get warmer and sea levels
to rise. The wave that forms then propagates east for several weeks, eventually
reaching South America and causing water off the coast to heat up and rise. An
El Niño develops as multiple Kelvin waves appear over the course of several
months, and the warm water accumulates off the shores of Colombia, Ecuador, and
Peru.
“While this year’s event started a
bit later than the big El Niños of 2015 and 1997, it’s beginning to catch up,”
said Josh Willis, a sea level researcher at NASA’s Jet Propulsion Laboratory in
Southern California and project scientist for Sentinel-6 Michael Freilich.
“We’ll see how big it gets.”
Measurements from Sentinel-6
Michael Freilich show a small Kelvin wave forming around Micronesia in late
January and dissipating by mid-February. A new wave emerged in early March,
then moved east over time. By mid-May, the seas around Peru were more than 5.9
inches (15 centimeters) higherthan long-term averages.
“NASA’s observation of El Niño uses
sea level satellites like Sentinel-6 Michael Freilich to track massive Kelvin
waves as they cross the Pacific, capture changes in Earth’s ocean
thermodynamics, improve forecasts of weather extremes, and help communities
prepare for potential coastal hazards,” said Nadya Vinogradova Shiffer, lead
program scientist at NASA Headquarters in Washington. “Stay tuned as more ocean
stories continue to unfold.”
Tracking El Niño
Fishermen in the 1600s coined the
name El Niño — Spanish for “the boy,” a reference to the birth of baby Jesus —
because it tended to intensify around Christmastime. Warmer waters meant they
would catch fewer fish.
Warmer sea surface temperatures in
the central and eastern Pacific affect atmospheric circulation patterns
worldwide by shifting the jet stream, which impacts storm tracks. This can lead
to heavy rain and snow in some areas and unusual heat and dryness in others.
How far away those impacts appear depends on the strength of the El Niño.
In more modest events, like the
ones that began in 2018 and 2023, impacts such as drought and flooding were
mostly seeb in and around the tropical Pacific. Large El Niños, like the one in
2015-2016, reach much farther, causing drought in Africa and flooding in
California.
El Niños usually peak between
November and January, so it will be several months before the largest impacts
become clear.
“Every El Niño is different,” said
JPL sea level researcher Severine Fournier, deputy project scientist for
Sentinel-6 Michael Freilich. “But they almost always make for a hot year and
big changes in rainfall in parts of the globe.”
Sentinel-6 Michael Freilich is the
current official reference satellite for global sea level measurements. Launched in
2020, it is continuing a legacy started in 1992 by the TOPEX/Poseidon
satellite. A series of successors have carried the baton since then, and the
latest, Sentinel-6B, which launched November 2025, will take over for its predecessor by the end of 2026.
More about Sentinel-6 Michael Freilich
Sentinel-6 Michael Freilich, named
after former NASA Earth Science Division Director Michael Freilich, is one of
two satellites that compose the Copernicus Sentinel-6/Jason-CS (Continuity of
Service) mission.
Sentinel-6/Jason-CS, a part of the
European Union’s Earth observation programme called Copernicus, was jointly
developed by ESA, the European Organisation for the Exploitation of
Meteorological Satellites (EUMETSAT), NASA, and the National Oceanic and Atmospheric
Administration (NOAA), with funding support from the European Commission and
technical support on performance from the French space agency CNES (Centre
National d’Études Spatiales). Spacecraft monitoring and control, as well as the
processing of all the altimeter science data, is carried out by EUMETSAT on
behalf of the European Union’s Copernicus Programme, with the support of all
partner agencies.
A division of Caltech in Pasadena,
JPL contributed three science instruments for each Sentinel-6 satellite:
the Advanced
Microwave Radiometer, the Global
Navigation Satellite System – Radio Occultation, and the Laser
Retroreflector Array. NASA also contributed launch services, ground systems supporting
operation of the NASA science instruments, the science data processors for two
of these instruments, and support for the U.S. members of the international
Ocean Surface Topography Science Team.
To learn more about Sentinel-6 Michael Freilich, visit: https://www.nasa.gov/sentinel-6
Source: NASA-European Sea Level Mission Homes in on El Niño - NASA

No comments:
Post a Comment