Sulfate Aerosol Forcing and Climate Change Seasonality

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Explore the impact of sulfate aerosols on seasonal climate change over mid-latitude oceans, uncovering strong seasonality in North Atlantic SST and the role of air-sea feedbacks. Discover the reasons behind sulfate aerosol seasonality, its radiative forcing effects, and contributions to sea surface temperature variabilit

  • Climate Change
  • Aerosols
  • Seas
  • Feedbacks
  • Research

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  1. The Role of Sulfate Aerosol Forcing and Air-Sea Feedbacks in Generating Strong Seasonality of Climate Change over the Mid-latitude Oceans Daniel Vimont1, Jack Zweifel, Sagar Rathod, Tristan L'Ecuyer, and David Henderson 1 University of Wisconsin-Madison, Contact: dvimont@wisc.edu EESD RGMA Project DE-SC0022029 Poster #104

  2. The Role of Sulfate Aerosol Forcing and Air-Sea Feedbacks in Generating Strong Seasonality of Climate Change over the Mid-latitude Oceans Daniel Vimont1, Jack Zweifel, Sagar Rathod, Tristan L'Ecuyer, and David Henderson 1 University of Wisconsin-Madison, Contact: dvimont@wisc.edu Since 1970, North Atlantic SST has warmed 50% faster during late SUMMER than late WINTER Sulfate aerosols are FIVE TIMES more abundant during SUMMER than WINTER despite no seasonality in SO2 emissions

  3. The Role of Sulfate Aerosol Forcing and Air-Sea Feedbacks in Generating Strong Seasonality of Climate Change over the Mid-latitude Oceans Daniel Vimont1, Jack Zweifel, Sagar Rathod, Tristan L'Ecuyer, and David Henderson 1 University of Wisconsin-Madison, Contact: dvimont@wisc.edu Why do sulfate aerosols exhibit strong seasonality? How does sulfate seasonality affect sulfate direct and cloud radiative forcing? How do the mean state, radiative forcing, and air-sea feedbacks contribute to SST seasonality? CESM2: SO4 Burden 1970 2010 US SO2 Emissions ? ???(?)? ?? = ?(?)? + ?(?) JANUARY W m-2 JULY Month kg m-2

  4. The Role of Sulfate Aerosol Forcing and Air-Sea Feedbacks in Generating Strong Seasonality of Climate Change over the Mid-latitude Oceans Daniel Vimont1, Jack Zweifel, Sagar Rathod, Tristan L'Ecuyer, and David Henderson 1 University of Wisconsin-Madison, Contact: dvimont@wisc.edu EESD RGMA Project DE-SC0022029 Poster #104

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