Nice “theory”. That might work if the Antarctic were merely not warming as fast as the Arctic. But it doesn’t explain why the Antarctic is getting colder.
The question is 'getting colder' for what reason and howlong the data is you selectively choose to cite. Did you research why and how temperatures fluctuate in Antarctica, or are you citing a selectively cite a layman's rag.
It is the Antarctic Circumpolar Current that isolates Antarctic and generally colder.
Not a nice theory what I described concerning Antarctica is fact. Actually the temperature fluctuations.of Antarctica are to great deal independent of the effects of global warming as described, and temperatures may vary over time for simply climatic cyclic reasons. Nonetheless in long term temperature variations the Antarctic are not immune to the effects of global warming.
Digest this and come back.
From:
https://doi.org/10.1029/2006GL027057
Climate
Antarctic temperatures over the past two centuries from ice cores
1. Introduction
[2] Given the enormous amount of freshwater stored in the Antarctic ice sheet and the impact that temperature changes may have on the ice sheet mass balance, it is important to understand how and why Antarctic temperatures have changed. Several studies have presented summaries of Antarctic temperature change based on instrumental records [e.g.,
Turner et al., 2005;
Jacka et al., 2004;
Vaughan et al., 2003]. The Antarctic Peninsula region has experienced some of the strongest surface warming on Earth during the past 50 years, while temperature trends across the continent differ in sign and magnitude among different time periods and seasons [
Turner et al., 2005]. Recent cooling across the continent in the summer and autumn has been linked to persistence of the positive index phase of the Southern Hemisphere Annular Mode (SAM) [
Thompson and Solomon, 2002]. The recent trend in the SAM has been attributed to various combinations of stratospheric ozone depletion and rising atmospheric CO2 concentrations [e.g.,
Thompson and Solomon, 2002;
Shindell and Schmidt, 2004], implying anthropogenic influences on Antarctic climate. However, the temporal variability of Antarctic climate is not well known, as continuous meteorological observations in the Antarctic began only in the late 1950s. Quantitative reconstruction of Antarctic temperatures has been faced with several challenges. First, the short and sparse instrumental observations make it difficult to determine how well variations in temperatures at research stations represent regional temperature variations across the continent. Second, while stable isotope time series from Antarctic ice cores are well‐known, reaching up to eight glacial cycles into the past [
EPICA Community Members, 2004], such records have generally not been available at the high‐resolution required for reconstructing the instrumental record. Finally, while statistical reconstruction approaches have been applied in regional to hemispheric‐scale reconstructions [e.g.,
Jones and Mann, 2004], such approaches have not been applied to Antarctic data.
[3] New data and improved understanding of the mechanisms explaining Antarctic temperature and stable isotope variations enable the quantitative reconstruction of Antarctic temperatures for the first time. Targeted ice‐coring projects, such as the International Trans‐Antarctic Scientific Expedition (ITASE), which has the specific objective of collecting numerous high‐resolution records, have greatly expanded the availability of proxy indicators of Antarctic climate [
Mayewski et al., 2006;
Steig et al., 2006]. The aim of this paper is to utilize these new data in a 200‐year‐long Antarctic temperature reconstruction (representing the main part of the continent) methodologically similar to temperature reconstructions covering other geographic regions.
2. Data
[4] For Antarctic surface temperature observations, we use the quality‐controlled station records from the Antarctic READER project, which archives continuous monthly observations covering generally the late 1950s to present [
Turner et al., 2004]. Time series from eight stations on the coast and the continental interior are included in our analysis, while data from the Peninsula region are excluded due to their location with respect to the main climatic pattern that dominates the continent (see Methods, below).
[5] Subannually‐resolved δ18O and δD (hereafter denoted “δ”) ice core records are compiled from Law Dome [
van Ommen et al., 2004], Siple Station [
Mosley‐Thompson et al., 1990], Dronning Maud Land (DML) [
Graf et al., 2002], and two West Antarctic sites of the United States component of ITASE [
Steig et al., 2006] (
Table 1). The Law Dome and DML records are stacks of several records from closely‐spaced sites in the region. These records have been well‐dated through counting of annual layers in ion‐chemistry and δ concentrations, and by the identification of volcanic eruption marker horizons. All isotopic data were referenced to the VSMOW and SLAP (Standard Light Antarctic Precipitation) standards from the International Atomic Energy Agency.