Abstract

The wintertime ENSO teleconnection over the North Pacific region consists of an intensified (weakened) low pressure center during El Nino (La Nina) events both in observations and in climate models. Here, it is demonstrated that this teleconnection persists too strongly into late winter and sprin... Show moreThe wintertime ENSO teleconnection over the North Pacific region consists of an intensified (weakened) low pressure center during El Nino (La Nina) events both in observations and in climate models. Here, it is demonstrated that this teleconnection persists too strongly into late winter and spring in the Community Earth System Model (CESM). This discrepancy arises in both fully coupled and atmosphere-only configurations, when observed SSTs are specified, and is shown to be robust when accounting for the sampling uncertainty due to internal variability. Furthermore, a similar problem is found in many other models from piControl simulations of the Coupled Model Intercomparison Project (23 out of 43 in phase 5 and 11 out of 20 in phase 6). The implications of this bias for the simulation of surface climate anomalies over North America are assessed. The overall effect on the ENSO composite field (El Nino minus La Nina) resembles an overly prolonged influence of ENSO into the spring with anomalously high temperatures over Alaska and western Canada, and wet (dry) biases over California (southwest Canada). Further studies are still needed to disentangle the relative roles played by diabatic heating, background flow, and other possible contributions in determining the overly strong springtime ENSO teleconnection intensity over the North Pacific. Show less