The anticipated Big Blow came unexpectedly in late October 2012, when a late-season tropical storm picked up enough energy from an unusually warm Atlantic Ocean to maintain hurricane intensity as it tracked north. Blocked from recurving eastwards by the Greenland High, Sandy “did something never observed before in records going back to 1851 – it
The anticipated Big Blow came unexpectedly in late October 2012, when a late-season tropical storm picked up enough energy from an unusually warm Atlantic Ocean to maintain hurricane intensity as it tracked north. Blocked from recurving eastwards by the Greenland High, Sandy “did something never observed before in records going back to 1851 – it