James D. Scott

2002: The atmospheric bridge: The influence of ENSO teleconnections on air–sea interaction over the global oceans (2009)

Michael A. Alexander, Ileana Bladé, Matthew Newman, John R. Lanzante, Ngar-cheung Lau, James D. Scott

During El Niño–Southern Oscillation (ENSO) events, the atmospheric response to sea surface temperature (SST) anomalies in the equatorial Pacific influences ocean conditions over the remainder of...

Climate Variability in a Coupled Atmosphere-Ocean Model: the Role of Ocean Mixed Layer Processes (2007)

Michael A. Alexander, James D. Scott, Clara Deser, Dr. Michael Alexander

A 50-year coupled atmosphere-ocean model integration is used to study sea surface temperature (SST) and mixed layer depth (h), and the processes which influence them. The model consists of an...

Elevated Ultraviolet-B Radiation Induces Cross-protection to Cold in Leaves of Rhododendron Under Field Conditions¶ (2004)

Linda Chalker-Scott, James D. Scott

Previously, we have shown a cold-hardening response in Rhododendron ‘English Roseum’ exposed to elevated ultraviolet-B radiation (UV-B, 280–320 nm) under growth chamber conditions. We have...

Winter-to-Winter Recurrence of Sea Surface Temperature, Salinity and Mixed Layer Depth Anomalies (2000)

Michael A. Alexander, Mike S. Timlin, James D. Scott, Special Issue, Beyond El, Niño Conference, ...

The mean seasonal cycle of mixed layer depth (MLD) in the extratropical oceans has the potential to influence temperature, salinity and mixed layer depth anomalies from one winter to the next....

Processes That Influence Sea Surface Temperature and Ocean Mixed Layer Depth Variability in a Coupled Model (2000)

Michael A. Alexander, James D. Scott, Clara Deser, Dr. Michael Alexander

A 50-year coupled atmosphere-ocean model integration is used to study sea surface temperature (SST) and mixed layer depth (h), and the processes which influence them. The model consists of an...