Fig. 4: Transient boreal summer response in surface temperature/winds/net downward heat flux and precipitation.
From: On the Atlantic extratropical-tropical teleconnection in response to external freshwater forcing
The response is the ensemble mean difference between the hosing and the control ensembles, averaged over boreal summer (JJAS) of years 01–10, 11–20, 21–30, and 31–40. a–d Surface temperature response (shading) overlapped with near-surface winds response (vector). e–h Net downward surface heat flux response. i–l Precipitation response.
