Subtropical High induced by an orbitally-driven decrease in Northern Hemisphere insolation. Future anthropogenic warming could result in a reversal of this trend, a northward migration of the North
Atlantic Subtropical High, and a return to year-round aridity in south-western Europe.
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- School of Geographical Sciences - Professor of Physical Geography
- Cabot Institute for the Environment
- The Bristol Research Initiative for the Dynamic Global Environment (BRIDGE)
Person: Academic , Member