December 05, 2003 The Measure of Water: NASA Creates New Map for the AtmosphereNASA scientists have opened a new window for understanding atmospheric water vapor, its implications for climate change and ozone depletion. Scientists have created the first detailed map of water, containing heavy hydrogen and heavy oxygen atoms, in and out of clouds, from the surface to some 25 miles above the Earth, to better understand the dynamics of how water gets into the stratosphere. Only small amounts of water reach the arid stratosphere, 10 to 50 kilometers (6 to 25 miles) above Earth, so any increase in the water content could potentially lead to destruction of some ozone-shielding capability in this part of the atmosphere. This could produce larger ozone depletions over the North and South Poles as well as at mid-latitudes. Water shapes Earth’s climate. The large amount of it in the lower atmosphere, the troposphere, controls how much sunlight gets through to the planet, how much is trapped in our skies, and how much goes back out to space. Higher in the stratosphere, where most of the Earth’s ozone shield protects the surface from harmful ultraviolet rays, there is very little water (less than .001 the surface concentration). Scientists don’t fully understand how air is dried before it gets to this region. In the troposphere, water exists as vapor in air, as liquid droplets in clouds, and as frozen ice particles in high altitude cirrus clouds. Since there is so much water closer to Earth and so little miles above, it is important to understand how water enters and leaves the stratosphere. The “isotopic content,” the natural fingerprint left by the heavy forms of water, is key to understanding the process. An isotope is any of two or more forms of an element having the same or very closely related chemical properties and the same atomic number, but different atomic weights. An example is oxygen 16 versus oxygen 18, both are oxygen, but one is heavier than the other. Heavy water is more readily condensed or frozen out from its vapor, causing the nature of its distribution to differ somewhat from the usual isotopic form of water. A measurement of the isotopic make-up of water vapor enables scientists to determine how water gets into the stratosphere. “For the first time, we have water isotope content mapped in incredible detail,” said Dr. Christopher R. Webster, a senior research scientist at NASA’s Jet Propulsion Laboratory (JPL),
Measuring water isotopes is extremely challenging, because they represent only a small fraction, less than one percent, of the total water in the atmosphere. Detailed measurements
“The laser technique gives us the ability to measure the different types of isotopes found in all water,” said Webster. “With the isotopic fingerprint, we discovered the ice particles found under the stratosphere were lofted from below, and some were grown there in place.” The data help explain how the water content of air entering the stratosphere is reduced, and show that gradual ascent and rapid upward motion associated with tall cloud systems (convective lofting) both play roles in establishing the dryness of the stratosphere. The purpose of the aircraft mission was to understand the formation, extent and processes associated with cirrus clouds. The mission used six aircraft from NASA and other federal
The mission was funded by NASA’s Earth Science Enterprise. The Enterprise is dedicated to understanding the Earth as an integrated system and applying Earth System Science to improve
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David E. Steitz
Alan Buis
This text derived from http://www.jpl.nasa.gov/releases/2003/164.cfm Recommend this Article to a Friend Back to: News |
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