Through analysis of previous winters it can be put forth that the most extreme winters (1890 and 2010) occur due to the absence of south-westerly winds and present discrete pressure patterns (Burgess and Klingaman, 2015). El-Niño should be considered as a possible factor for the fluctuations of climate in the UK because tropical convection occurs in the tropical Pacific region (where El- Niño happens), which controls the distribution of heat globally driving atmospheric temperatures. However because of the geographical differences of where El- Niño occurs in association to the UK the magnitude of such impacts are less dominant than what the media
Through analysis of previous winters it can be put forth that the most extreme winters (1890 and 2010) occur due to the absence of south-westerly winds and present discrete pressure patterns (Burgess and Klingaman, 2015). El-Niño should be considered as a possible factor for the fluctuations of climate in the UK because tropical convection occurs in the tropical Pacific region (where El- Niño happens), which controls the distribution of heat globally driving atmospheric temperatures. However because of the geographical differences of where El- Niño occurs in association to the UK the magnitude of such impacts are less dominant than what the media