TY - JOUR
T1 - Twelve years of change in coastal upwelling along the central-northern coast of Chile
T2 - Spatially heterogeneous responses to climatic variability
AU - Aravena, Guillermo
AU - Broitman, Bernardo
AU - Stenseth, Nils Christian
PY - 2014/2/28
Y1 - 2014/2/28
N2 - We use time-series analyses to characterize the effects of recent climate variability upon the local physical conditions at 11 study sites along the northern-central coast of Chile (29-34uS). Environmental indices show that the 1u Bakun upwelling index in this coastal region has fluctuated in time, starting from a stable period around the 1980's, peaking during the mid 90s, decreasing during the next ten years and increasing at a steep rate since 2010. Upwelling intensity decreased with increasing latitude, showing also a negative correlation with climate patterns (El Nino3 sea surface temperature-SST anomalies and the Multivariate El Nino Index). We hypothesize that the impacts of climate variability on upwelling events seem to be spatially heterogeneous along the region. Non-sheltered locations and, particularly, sites on prominent headlands show an immediate (lag = 0) and negative correlation between local SST, upwelling events and wind stress. We suggest that near-shore thermal conditions are closely coupled to large-scale forcing of upwelling variability and that this influence is modulated through local topographic factors.
AB - We use time-series analyses to characterize the effects of recent climate variability upon the local physical conditions at 11 study sites along the northern-central coast of Chile (29-34uS). Environmental indices show that the 1u Bakun upwelling index in this coastal region has fluctuated in time, starting from a stable period around the 1980's, peaking during the mid 90s, decreasing during the next ten years and increasing at a steep rate since 2010. Upwelling intensity decreased with increasing latitude, showing also a negative correlation with climate patterns (El Nino3 sea surface temperature-SST anomalies and the Multivariate El Nino Index). We hypothesize that the impacts of climate variability on upwelling events seem to be spatially heterogeneous along the region. Non-sheltered locations and, particularly, sites on prominent headlands show an immediate (lag = 0) and negative correlation between local SST, upwelling events and wind stress. We suggest that near-shore thermal conditions are closely coupled to large-scale forcing of upwelling variability and that this influence is modulated through local topographic factors.
UR - http://www.scopus.com/inward/record.url?scp=84896522075&partnerID=8YFLogxK
U2 - 10.1371/journal.pone.0090276
DO - 10.1371/journal.pone.0090276
M3 - Article
C2 - 24587310
AN - SCOPUS:84896522075
SN - 1932-6203
VL - 9
JO - PLoS ONE
JF - PLoS ONE
IS - 2
M1 - e90276
ER -