Recovery of the boreal forest after a long period of deforestation will require sustained warming which, indeed, has currently been taking place since the mid-1990s in
Eastern subarctic Canada.
Climate variability and change in the Canadian
Eastern Subarctic IRIS region (Nunavik and Nunatsiavut).
Not exact matches
Summary: Temperature and sea ice «abberations» in northern Greenland are transient phenomena that have clearly happened before (e.g. 2011) without major consequences except perhaps through impacts on
eastern Arctic and
subArctic weather conditions (including the UK).