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Title: A 3D View of an Atmospheric River from an Earth System Model
Features in Earth’s atmosphere,
spawned by the heat of the Sun and the rotation of the Earth,
transport water and energy around the globe.
Clouds and precipitation shown here are from NASA’s MERRA-2 reanalysis,
a retrospective blend of a weather model
and conventional and satellite observations.
Within the mid-latitudes, winds move clouds from west to east.
Within the tropics easterly trade winds converge
along the equator to create a moisture rich cluster
of clouds, convection, and precipitation called the
intertropical convergence zone, or ITCZ.
Disturbances in its flow transport immense amounts of moisture
and energy from the tropics to the poles.
Studies have shown that atmospheric rivers account for the vast majority
of the poleward transport of water vapor.
The American Meteorological Society defines an atmospheric river
as “a long, narrow, and transient corridor of
strong horizontal water vapor transport that is typically associated
with a low-level jet stream ahead of the cold front of an extratropical cyclone.”
A common measure for the strength of an atmospheric river
is the integrated water vapor transport, or the amount of moisture
that is moved from one place to another by the flow of the atmosphere.
The blue shading shown here gives a three-dimensional view
of the water vapor transport.
Tropical moisture is pulled in from the ITCZ
and in this example, converges with other flows to form an atmospheric river.
The feature then travels towards the west coast of the United States
as a sub-class of atmospheric rivers commonly referred to
as the “pineapple express” due to its origin near Hawai’i.
The atmospheric river is guided
guided by the semi-permanent sub-tropical high pressure off the coast of California
and the Baja Peninsula as well as
the Aleutian low in the Gulf of Alaska.
The pressure gradient between the clockwise flow of the Californian high
and the counterclockwise flow of the Aleutian low funnel the atmospheric moisture into a narrow corridor.
The more intense the pressure gradient is,
the stronger the winds are that transport the water vapor.
Extreme rainfall has also been associated with the more intense gradients.
Much of the moisture stays close to the surface
but the rising motion of the low pressure to the north
results in the air cooling, condensing the water vapor into a liquid.
Precipitation over the ocean falls along the feature’s cold front on its northern side.
Another way that air can rise
and condense into precipitation is through orographic lift.
When air encounters the mountains
along the west coast of the United States, it is forced upwards.
The rising air becomes saturated, causing rain and snow to fall,
particularly on the windward side of the mountain.
The flow of air continues eastward, depleted of its moisture.
The precipitation that falls because of atmospheric rivers
is important for the hydrologic cycle in the western United States.
The winter buildup of the snowpack provides valuable freshwater resources.
Despite being beneficial at times,
, atmospheric river induced precipitation can also be destructive.
The occurrence of extreme atmospheric river precipitation events,
such as the one that occurred in this example,
can result in widespread flooding and mudslides.
Atmospheric rivers are not unique to the west coast of North America
and occur around the globe, including New Zealand,
Greenland, Antarctica, and the Middle East.
The study of global phenomenon such as atmospheric rivers over the past four decades
decades is made possible through NASA’s MERRA-2 reanalysis,
, a spatially and temporally consistent blend of satellite
and conventional observations with a numerical model.
With a dataset that provides hourly information
around the globe since 1980,
there is still much that can be learned about Earth’s atmosphere
and the transport of water and energy around the globe.
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