Statistical analysis and time-series models for minimum/maximum temperatures in the Antarctic Peninsula

It is now widely known that Antarctic air is warming faster than the rest of the world, and theAntarcticPeninsula has experiencedmajorwarming over the last 50years.Themonthly mean near surface temperature at the Faraday/Vernadsky station has increased considerably, at a rate of 0.568C per decade over the year and at 1.098C per decade over thewinter. The increase is not the same over all the stations in theAntarctic region, and the increase is very significant at the Faraday/Vernadsky station. Only at this station are the minimum/maximum monthly temperatures, for the period 1951–2004, separately available, and we believe that the increase in mean surface temperature at this station is mainly due to the increases inminimum temperatures. Therefore, our object in this paper is to study the variations in the minimum/maximum temperatures using a multiple regression model with non-Gaussian correlated errors. By separately analysing the minimum and maximum temperatures, we could clearly identify the source of increase. The average temperature (usually calculated as (maxCmin)/2) smooths out any variation, and may not be that informative. We model the correlated errors using a linear autoregressive moving average model with innovations, which have an extreme value distribution.We describe the maximum-likelihood estimation methodology and apply this to the datasets described earlier. The methods proposed here can be widely used in other disciplines as well. Our analysis has shown that the increase in the minimum monthly temperatures is approximately 6.78C over 53 years (1951–2003), whereas we did not find any significant change in themaximumtemperature over the sameperiod.Wealso establish a relationship between the minimum monthly temperatures and ozone levels, and use this model to obtain monthly forecasts for the year 2004 and compare it with the true values available up to December 2004.