Now showing items 1-2 of 2
The impact of mean state errors on equatorial Atlantic interannual variability in a climate model
(American Geophysical Union, 2015-02-23)
Observations show that the Equatorial Atlantic Zonal Mode (ZM) obeys similar physics to the El Niño Southern Oscillation (ENSO): positive Bjerknes and delayed negative feedbacks. This implies the ZM may be predictable on ...
Water mass transformation and the North Atlantic Current in three multi-century climate model simulations
(American Geophysical Union, 2012-11)
The warm and saline Subtropical Water carried by the North Atlantic Current undergoes substantial transformation on its way to higher latitudes as heat is released from ocean to atmosphere. The geographical distribution ...