Contrails - Research, comments and linksContrails and Aviation-induced Cirrus CloudsNASA (01)https://www.nasa.gov/home/hqnews/2004/apr/HQ_04140_clouds_climate.html
Clouds Caused By Aircraft Exhaust May Warm The U.S. Climate "This result shows the increased cirrus coverage, attributable to air traffic, could account for nearly all of the warming observed over the United States for nearly 20 years starting in 1975, but it is important to acknowledge contrails would add to and not replace any greenhouse gas effect," said Patrick Minnis, senior research scientist at NASA's Langley Research Center in Hampton, Va. The study was published April 15 in the Journal of Climate. "During the same period, warming occurred in many other areas where cirrus coverage decreased or remained steady," he added. "This study demonstrates that human activity has a visible and significant impact on cloud cover and, therefore, on climate. It indicates that contrails should be included in climate change scenarios," Minnis said. Minnis determined the observed one percent per decade increase in cirrus cloud cover over the United States is likely due to air traffic-induced contrails. Using published results from NASA's Goddard Institute for Space Studies (New York) general circulation model, Minnis and his colleagues estimated contrails and their resulting cirrus clouds would increase surface and lower atmospheric temperatures by 0.36 to 0.54 degrees Fahrenheit per decade. Weather service data reveal surface and lower atmospheric temperatures across North America rose by almost 0.5 degree Fahrenheit per decade between 1975 and 1994. Minnis worked with colleagues Kirk Ayers, Rabi Palinkonda, and Dung Phan from Analytical Services and Materials, Inc., of Hampton, Va. They used 25 years of global surface observations of cirrus clouds, temperature and humidity records from the National Centers for Environmental Prediction (NCEP) reanalysis dataset. They confirmed the cirrus trends with 13 years of satellite data from NASA's International Satellite Cloud Climatology Project. Both air traffic and cirrus coverage increased during the period of warming despite no changes in the NCEP humidity at jet cruise altitudes over the United States. By contrast, humidity at flight altitudes decreased over other land areas, such as Asia, and was accompanied by less cirrus coverage, except over Western Europe, where air traffic is very heavy. Cirrus coverage also rose in the North Pacific and North Atlantic flight corridors. The trends in cirrus cover and warming over the United States were greatest during winter and spring, the same seasons when contrails are most frequent. These results, along with findings from earlier studies, led to the conclusion that contrails caused the increase in cirrus clouds. "This study indicates that contrails already have substantial regional effects where air traffic is heavy, such as over the United States. As air travel continues growing in other areas, the impact could become globally significant," Minnis said. Humidity is the amount of water vapor in the air and determines how long contrails remain in the atmosphere. Contrails that persist for an extended period of time are most likely to impact the climate. Contrails form high in the atmosphere when the mixture of water vapor in the aircraft exhaust and the air condenses and freezes. Persisting contrails can spread into extensive cirrus clouds that tend to warm the Earth, because they reflect less sunlight than the amount of heat they trap. The balance between Earth's incoming sunlight and outgoing heat drives climate change. NASA's Earth Science Enterprise funded this research. NASA's Earth Science Enterprise is dedicated to understanding the Earth as an integrated system and applying Earth System Science to improve prediction of climate, weather, and natural hazards using the unique vantage point of space. For information about this research on the Internet, visit:
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https://www.nasa.gov/home/index.html Langley Technical Report Server Patrick Minnis, J. Kirk Ayers and Steven P. Weaver, Surface-Based Observations of Contrail Occurrence Frequency Over the U.S., April 1993--April 1994 , NASA RP-1404, December 1997, pp. 83, (4MB). Format(s): Postscript, or PDF Keywords: Contrails; Cirrus clouds; Surface observation; Subsonic assessment; Aircraft effects; Climate change Abstract: Surface observers stationed at 19 U.S. Air Force Bases and
Army Air Stations recorded the daytime occurence of contrails and cloud fraction on an
hourly basis for the period April 1993 through April 1994. Each observation uses one of
four main categories to report contrails as unobserved, non-persistent, and indeterminate.
Additional classification includes the co-occurence of cirrus with each report. The data
cover much of the continental U.S. including locations near major commercial air routes.
The mean annual frequency of occurrence in unobstructed viewing conditions is 13 percent
for these sites. Contrail occurrence varied substantially with location and season. Most
contrails occurred during the winter months and least during the summer with a pronounced
minimum during July. Although nocturnal observations are not available, it appears that
the contrails have a dirunal variation that peaks during mid morning over most areas.
Contrails were most often observed in areas near major commerical air corridors and least
often over areas far removed from the heaviest air traffic. A significant correlation
exists between mean contrail frequency and aircraft fuel usage above 7 km suggesting
predictive potential for assessing future contrail effects on climate. Long tracks of exhaust left behind by commercial jetsJuly 27 What happens to the long tracks of exhaust left behind by commercial jets? NASA scientists are discovering that some of those tracks, known as contrails, linger for hours and actually become clouds. NBCs Robert Hager reports on the phenomenon and what it may mean for our global climate. NASA RESEARCHER Patrick Minnis studied satellite photos of the airplane jetstreams, which occur only when the sky is
moist, close to forming thin clouds. What he discovered may sound far-fetched but
the evidence is clear.
Spreading and Growth of Contrails in a Sheared Environment Atmospheric Physics BranchThe evolution of persistent contrails has modeled over time-scales of 15-180 minutes using a large-body simulation model with detailed microphysics. Model results have been compared to satellite and in situ measurements of persistent contrails from the SUCCESS experiment. In particular, we simulated the evolution of the persistent contrail observed on May 12, 1996. In simulations with large ambient supersaturations and moderate wind shear, crystals with length > 200 microns are generated within 35 minutes by depositional growth. In situ measurements in the May 12 contrail case showed that these large crystals did in fact form. The large crystals fall rapidly and the contrail horizontal extent increases due to the wind shear (see Figure 1). Strong radiative heating (with rates up to 30 K/day) drives a local updraft and lofts the contrail core several hundred meters. FS-2000-04-010-GRC
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