FN Archimer Export Format PT J TI A new climate index controlling winter wave activity along the Atlantic coast of Europe: The West Europe Pressure Anomaly BT AF CASTELLE, Bruno DODET, Guillaume MASSELINK, Gerd SCOTT, Tim AS 1:1,2;2:3;3:4;4:4; FF 1:;2:;3:;4:; C1 CNRS, UMR EPOC, Pessac, France. Univ Bordeaux, UMR EPOC, Pessac, France. Inst Univ Europeen Mer UBO, LETG Brest Geomer UMR CNRS 6554, Plouzane, France. Univ Plymouth, Sch Biol & Marine Sci, Coastal Proc Res Grp, Plymouth, Devon, England. C2 CNRS, FRANCE UNIV BORDEAUX, FRANCE UBO, FRANCE UNIV PLYMOUTH, UK IF 4.339 TC 85 UR https://archimer.ifremer.fr/doc/00606/71850/70485.pdf https://archimer.ifremer.fr/doc/00606/71850/70486.txt LA English DT Article AB A pioneering and replicable method based on a 66-year numerical weather and wave hindcast is developed to optimize a climate index based on the sea level pressure (SLP) that best explains winter wave height variability along the coast of western Europe, from Portugal to UK (36-52 degrees N). The resulting so-called Western Europe Pressure Anomaly (WEPA) is based on the sea level pressure gradient between the stations Valentia (Ireland) and Santa Cruz de Tenerife (Canary Islands). The WEPA positive phase reflects an intensified and southward shifted SLP difference between the Icelandic low and the Azores high, driving severe storms that funnel high-energy waves toward western Europe southward of 52 degrees N. WEPA outscores by 25-150% the other leading atmospheric modes in explaining winter-averaged significant wave height, and even by a largest amount the winter-averaged extreme wave heights. WEPA is also the only index capturing the 2013/2014 extreme winter that caused widespread coastal erosion and flooding in western Europe. PY 2017 PD FEB SO Geophysical Research Letters SN 0094-8276 PU Amer Geophysical Union VL 44 IS 3 UT 000396115000024 BP 1384 EP 1392 DI 10.1002/2016GL072379 ID 71850 ER EF