Spatial analysis of trends in primary production and relationship with large‐scale climate variability in the Ross Sea, Antarctica (1997–2013)

Recent studies have documented an increase in sea ice extent and the duration of the ice season in the Ross Sea, Antarctica. We conducted a satellite‐based study to quantify changes in net primary production (NPP) and chlorophyll a (Chl a) in response to the observed changes in ice dynamics in the Ross Sea south of 60°S. Our study covers a 16 year time period (1997–2013) and incorporates both the shelf and off‐shelf regions of the Ross Sea. We observed significant secular changes in NPP from 1997 to 2013 in the off‐shelf region, with NPP increasing on the eastern side and decreasing on the western side of our study area. The changes we observed in NPP are consistent with the changes we observed in sea surface temperature (SST) and open water days (OWDs), decreasing (increasing) on the western (eastern) side of our study area. Finally, we examined the influence of the Southern Annular Mode (SAM) and the El Niño Southern Oscillation (ENSO), on SST, OWDs, Chl a, and NPP in the Ross Sea and observed a significant relationship between the state of the SAM and ENSO and SST, OWDs, and NPP across the study region. The response of OWDs, SST, and NPP to atmospheric forcing by SAM and ENSO was opposite for the shelf and off‐shelf regions, such that during a positive phase of SAM or negative phase of ENSO (La Niña), SST, OWDs, and NPP increased on the shelf and decreased in the off‐shelf region. Key Points: Secular change in NPP off the shelf tracks changes in OWDs and SST Response of OWDs and NPP to SAM and ENSO was opposite for the shelf and off‐shelf regions