![Figure 3: Precipitation responses (unit: mm/day) to uniform SST warming from FLOR‐A06 (top row) and CM2.6 (bottom row). Shown from left to right are total, large‐scale, and convective precipitation changes. Contours show the climatological P − E in (a) and (b), climatological large‐scale precipitation in (c) and (d), and climatological convective precipitation in (e) and (f). All climatological field are calculated from the AMIP_ctrl simulation. Contour interval is 0.5 mm/day. Dashed contours indicate negative values. Zero contours are thickened. SST = sea surface temperature; FLOR = Forecast Low Ocean Resolution.](https://i0.wp.com/idsc.miami.edu/wp-content/uploads/2020/12/Impact-of-Ocean-Eddy-figure-3-940x530-1.jpg?resize=730%2C350&ssl=1)
Impact of Ocean Eddy Resolution on the Sensitivity of…
Global coupled atmosphere‐ocean models have not included the explicit simulation of ocean mesoscale eddies (turbulent ocean flow with a horizontal scale of less than 100 km) until the recent few years. As a result, current estimates of precipitation responses to greenhouse gases increase have predominantly relied on models in which ocean eddies have to be parameterized. Read more “Impact of Ocean Eddy Resolution on the Sensitivity of Precipitation to CO2 Increase”