Cloudy With A Chance of Warming
Clouds can increase warming in the changing Arctic region more than scientists expected, by delivering an unexpected double-whammy to the climate system, according to a new study by researchers at NOAA, the University of Colorado Boulder and colleagues.
“As the Arctic atmosphere warms and moistens, it better insulates the surface. While we expected this to reduce the insulating influence of clouds, we found that Arctic clouds forming in these conditions appear to further warm the surface, especially in the fall and winter,” said Christopher Cox, lead author of the new paper published today in Nature Communications. Cox is a research scientist with the Cooperative Institute for Research in Environmental Sciences (CIRES), who works at NOAA’s Earth System Research Laboratory in Boulder, Colorado.
Clouds are a complicated character in the climate change story: Sometimes they cool the planet’s surface by reflecting sunlight, sometimes they insulate it and keep it warm.
“To understand why and where Earth is warming, you have to understand clouds,” Cox said.
Head north to the Arctic, and clouds’ impact on climate is particularly difficult to understand, he said. The amount and manner in which clouds warm the surface is determined by an intricate dance between moisture (relative humidity), temperatures and the properties of the clouds—and that dance “is different in the Arctic, where the air is colder and drier than at lower latitudes,” Cox said.
To nail down the overarching influence of Arctic clouds on temperatures, he and colleagues from CIRES, NOAA, Washington State University, Idaho and Chile analyzed measurements from three science research stations in the far north: Barrow, Alaska; Eureka, Canada; and Summit, Greenland.
They assessed things like temperature, relative humidity, and a measure of the cloud insulating properties (“the downwelling infrared cloud radiative effect”), and they looked at how those factors interacted with one another (in different parts of the infrared spectrum).
Previous work suggested that as the atmosphere itself warms and becomes more moist it becomes a better insulator, so the clouds themselves have a diminishing contribution to warming. This is likely true on a global scale: It’s as if a person is already warm under a blanket and adding another blanket has little additional effect.
However, this team found a different behavior when temperature and humidity increase in the cold Arctic. There, clouds can retain their ability to warm the surface, and actually appear to be amplifying regional warming. In this cold, dry region, adding a second “blanket” can, in fact, make it even warmer.
The effect—strongest in autumn and winter—is related to the way that temperature and moisture are changing relative to each other in the region, according to the new analysis, which relied on climate modeling as well as observations. Because there is little sunlight in the Arctic in autumn and winter, the insulating properties of clouds far outweigh their shading properties, making this result all the more important, said co-author Matthew Shupe, also a CIRES researcher who works at NOAA.
He and his colleagues said their findings call for better monitoring of changes in the Arctic atmosphere, including temperature and moisture levels as well as cloud properties, and continued work to improve the representation of clouds in computer models designed to understand the rapidly evolving Arctic region.
“We’re seeing what climate change in the Arctic looks like," said co-author Von P. Walden of Washington State University. "As we go forward in time, it is essential to better understand how the humidity changes in a warmer atmosphere. This is key to understanding how clouds warm the surface."
Authors of “Humidity trends imply increased sensitivity to clouds in a warming Arctic” in Nature Communications are Christopher J. Cox (CIRES and NOAA), Von P. Walden (Washington State University), Penny M. Rowe (University of Idaho and Universidad de Santiago de Chile) and Matthew D. Shupe (CIRES and NOAA). This work was supported by the NOAA Climate Program Office (CPO) Arctic Research Program, the CIRES Visiting Fellows Program, the National Science Foundation (NSF), Fondo Nacional de Desarrollo Científico y Tecnológico (FONDECYT, of Chile), Dirección de Investigación Científica y Tecnológica (Dicyt, of Chile), and the U.S. DOE Atmospheric Radiation Measurement (ARM) Program.