Figure 3: Observed versus modelled time series of chl-a at Palmer Stations B and E.
From: Winter and spring controls on the summer food web of the coastal West Antarctic Peninsula
A stepwise regression of General Linear Models (GLMs) combined with model ranking criteria identified the predictor variables and their interactions that constrain the average log-transformed summer (December–January–February) depth-integrated (0–50 m) phytoplankton biomass at Palmer Station B (a; Pearson’s R=0.96, adjusted r2=0.67) and E (b; Pearson’s R=0.86, adjusted r2=0.54) in each summer. (See text and Supplementary Tables 1 and 2 for details on the model equations, predictors and statistics.)
