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A groundbreaking study explores the intricate link between Earth’s surface temperature and outgoing longwave radiation, revealing deviations from the expected quartic pattern. This research enhances our comprehension of climate sensitivity and the factors influencing it, such as greenhouse gases and atmospheric dynamics. Credit: SciTechDaily.com
Research in climate science reveals new insights into the relationship between surface temperature and outgoing longwave radiation, challenging conventional models and deepening our understanding of Earth’s climate sensitivity.
Curious about what drives Earth’s climate sensitivity? A recent study in Advances in Atmospheric Sciences explores the complex links transforming the relationship between surface temperature and outgoing longwave radiation (OLR) from quartic to quasi-linear. Led by Dr. Jie Sun from
Diagram depicting the two main processes for quasi-linear surface temperature and outgoing longwave radiation (OLR). Left: enhancement of meridional surface temperature gradient by the greenhouse effect of water vapor; Right: Re-routing part of OLR from warm places to cold places by poleward energy transport. Credit: Ming Cai and Xiaoming Hu
Factors Influencing Surface Temperature and OLR
The study uncovers how various factors influence surface temperature and OLR. The greenhouse effect of water vapor acts as a magnifier, amplifying temperature differences across Earth’s surface without altering the latitudinal variation of OLR. This suppresses the nonlinearity between OLR and surface temperature.
Poleward energy transport, on the other hand, functions as an equalizer, harmonizing temperature disparities across different regions of the globe. One of the by-products of this global heat redistribution is the re-routing of OLR from warm places to cold places, acting to reduce OLR difference across different regions. This, in turn, further suppresses the nonlinearity.
Prof. Ming Cai from Florida State University highlighted, “Understanding these complex climate interactions is akin to decoding a puzzle. Each piece brings us closer to deciphering our planet’s climate intricacies.”
By illuminating these connections, scientists make significant strides in comprehending Earth’s climate and how its intricate components orchestrate the overall climate sensitivity, namely not only energy output rate but also where the output takes place.
Reference: “A Quasi-Linear Relationship between Planetary Outgoing Longwave Radiation and Surface Temperature in a Radiative-Convective-Transportive Climate Model of a Gray Atmosphere” by Jie Sun, Michael Secor, Ming Cai and Xiaoming Hu, 25 November 2023, Advances in Atmospheric Sciences.
DOI: 10.1007/s00376-023-2386-1