Monday, December 15, 2014

NASA MAVEN: Links in Chain Leading to Atmospheric Loss Identified

NASA’s MAVEN mission is observing the upper atmosphere of Mars to help understand climate change on the planet. 

MAVEN entered its science phase on Nov. 16, 2014.

Image Credit: NASA's Goddard Space Flight Center

Early discoveries by NASA’s newest Mars orbiter are starting to reveal key features about the loss of the planet’s atmosphere to space over time.

The findings are among the first returns from NASA’s Mars Atmosphere and Volatile Evolution (MAVEN) mission, which entered its science phase on Nov. 16.

The observations reveal a new process by which the solar wind can penetrate deep into a planetary atmosphere.

They include the first comprehensive measurements of the composition of Mars’ upper atmosphere and electrically charged ionosphere.

The results also offer an unprecedented view of ions as they gain the energy that will lead to their to escape from the atmosphere.

“We are beginning to see the links in a chain that begins with solar-driven processes acting on gas in the upper atmosphere and leads to atmospheric loss,” said Bruce JakoskyMAVEN principal investigator with the Laboratory for Atmospheric and Space Physics at the University of Colorado, Boulder.

“Over the course of the full mission, we’ll be able to fill in this picture and really understand the processes by which the atmosphere changed over time.”

On each orbit around Mars, MAVEN dips into the ionosphere, the layer of ions and electrons extending from about 75 to 300 miles above the surface.

This layer serves as a kind of shield around the planet, deflecting the solar wind, an intense stream of hot, high-energy particles from the sun.

Scientists have long thought that measurements of the solar wind could be made only before these particles hit the invisible boundary of the ionosphere.

The SWIA instrument will measure the solar wind and ion density and velocity in the magnetosheath of Mars. 

Credit: UCB/SSL

MAVEN’s Solar Wind Ion Analyzer (SWIA), however, has discovered a stream of solar-wind particles that are not deflected but penetrate deep into Mars’ upper atmosphere and ionosphere.

Interactions in the upper atmosphere appear to transform this stream of ions into a neutral form that can penetrate to surprisingly low altitudes.

Deep in the ionosphere, the stream emerges, almost Houdini-like, in ion form again.

The reappearance of these ions, which retain characteristics of the pristine solar wind, provides a new way to track the properties of the solar wind and may make it easier to link drivers of atmospheric loss directly to activity in the upper atmosphere and ionosphere.

The NGIMS instrument will measure the composition and isotopes of thermal neutrals and ions in the Martian atmosphere. 


MAVEN’s Neutral Gas and Ion Mass Spectrometer (NGIMS) is exploring the nature of the reservoir from which gases are escaping by conducting the first comprehensive analysis of the composition of the upper atmosphere and ionosphere.

These studies will help researchers make connections between the lower atmosphere, which controls climate, and the upper atmosphere, where the loss is occurring.

The instrument has measured the abundances of many gases in ion and neutral forms, revealing well-defined structure in the upper atmosphere and ionosphere, in contrast to the lower atmosphere, where gases are well-mixed.

The variations in these abundances over time will provide new insights into the physics and chemistry of this region and have already provided evidence of significant upper-atmospheric “weather” that has not been measured in detail before.

The STATIC instrument will enable measurement of energetic particles in the Martian atmosphere. Credit: NASA/SSL

New insight into how gases leave the atmosphere is being provided by the spacecraft’s Suprathermal and Thermal Ion Composition (STATIC) instrument.

Within hours after being turned on at Mars, STATIC detected the “polar plume” of ions escaping from Mars.

This measurement is important in determining the rate of atmospheric loss.

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