hat
Tanpèt gwo ka aktyèlman ap benefisye resif koray. Pou egzanp, siklòn ka diminye klowòks koray pa sa ki lakòz rediksyon kout tèm nan tanperati lanmè lokal yo, konsa diminye estrès tèmik. ref Siklòn kapab tou redwi abondans nan koloni koray pi sansib a estrès tèmik, (egzanp, branch ak koloni tabula) ki ka domine resif ki raman eksperyans tanpèt, konsa diminye potansyèl la pou tanpèt nan lavni lakòz plis domaj. Tanpèt twopikal kapab tou pou yon ti tan retire twòp macroalga, ki ka mete restriksyon sou rekritman koray ak kwasans, byenke domaj pòs-siklòn nan kouvèti koray ak vibran nan eleman nitritif ka mennen nan orè nan kominote alg-domine. ref Klèman konbinezon de domaj ak refwadisman ka jwe yon wòl enpòtan nan dinamik Reef. ref
eng
Large storms can actually be beneficial to coral reefs. For example, hurricanes can mitigate coral bleaching by causing short-term reductions in local sea temperatures, thus reducing thermal stress. ref Hurricanes can also reduce the abundance of coral colonies more susceptible to thermal stress, (e.g., branching and tabular colonies) which can dominate reefs that rarely experience storms, thus reducing the potential for future storms to cause further damage. Tropical storms can also temporarily remove excessive macroalgae, which can restrict coral recruitment and growth, although post-hurricane damage to coral cover and stirring of nutrients may lead to shifts to algal-dominated communities. ref Clearly the combination of damage and cooling can play an important role in reef dynamics. ref