Wind-driven coastal circulation in the Gulf of Tehuantepec, Mexico ...

Ciencias Marinas, Vol. 37, No. 4A, 2011Barton ED, Lavín MF, Trasviña A. 2009. Coastal circulation andhydrography in the Gulf of Tehuantepec, Mexico, during winter.Cont. Shelf Res. 29: 485–500.Clarke AJ. 1988. Inertial wind path and sea surface temperaturepatterns near the Gulf of Tehuantepec and Gulf of Papagayo.J. Geophys. Res. 93(C12): 15491–15501.Chelton DB, Esbensen SK, Schlax MG, Thum N, Freilich MH,Wentz FJ, Gentemann CL, McPhaden MJ, Schopf PS. 2001.Observations of coupling between surface wind stress and seasurface temperature in the Eastern Tropical Pacific. J. Clim. 14:1479–1498.Flores-Vidal X, Durazo R, Flament P, Chavanne C. 2011.Circulación costera en ausencia de viento en el Golfo deTehuantepec, México: Observaciones con radares de altafrecuencia. Cienc. Mar. 37(4A): 493–512.González-Silvera A, Santamaría-del-Ángel E, Millán-Núñez R,Manzo-Monroy H. 2004 Satellite observations of mesoscaleeddies in the gulfs of Tehuantepec and Papagayo (EasternTropical Pacific). Deep-Sea Res. II 51: 587–600.Gurgel KW, Antonischki G, Essen HH, Schlick T. 2000. WellenRadar (WERA): A new ground-wave HF radar for ocean remotesensing. Coast. Eng. 37: 219–234.Hoffman RN. 1984. SASS wind ambiguity removal by directminimization. Mon. Weather Rev. II 112: 1829–1852.Kessler WS. 2002. Mean three-dimensional circulation in theNortheast Tropical Pacific. J. Phys. Oceanogr. 32: 2457–2471.Large WG, Pond S. 1981. Open ocean momentum flux measurementsin moderate to strong winds. J. Phys. Oceanogr. 11:324–336.Lavín MF, Robles JM, Argote ML, Barton ED, Smith R, Brown J,Kosro M, Trasviña A, Vélez HS, García J. 1992. Física delGolfo de Tehuantepec. Cienc. Desarr. VXVIII(103): 98–108.McClain CR, Christian JR, Signorini SR, Lewis MR, Asanuma I,Turk D, Dupouy-Douchement C. 2002. Satellite ocean-colorobservations of the tropical Pacific Ocean. Deep-Sea Res. II 49:2533–2560.McCreary JP, Lee HS, Enfield DB. 1989. The response of the coastalocean to strong offshore winds: With application to circulationsin the gulfs of Tehuantepec and Papagayo. J. Mar. Res. 47:81–109.Müller-Karger FE, Fuentes-Yaco C. 2000. Characteristics of windgeneratedrings in the eastern tropical Pacific Ocean. J. Geophys.Res. 105(C1): 1271–1284.Paduan J, Cook M. 2004. HFRadarmap toolbox for MATLAB,Naval Postgraduate School, Monterey, California (available athttp://www.oc.nps.navy.mil/radlab/HFRadarmapToolbox/).Romero-Centeno R, Zavala-Hidalgo J, Gallegos A, O’Brien JJ.2003. Isthmus of Tehuantepec wind climatology and ENSOsignal. J. Clim. 16: 2628–2639.Steenburgh WJ, Schultz DM, Colle BA. 1998. The structure andevolution of gap outflow over the Gulf of Tehuantepec, Mexico.Mon. Weather Rev. 126: 2673–2691.Stumpf HG. 1975. Satellite detection of upwelling in the Gulf ofTehuantepec, Mexico. J. Phys. Oceanogr. 5: 383–388.Stumpf HG, Legeckis RV. 1977. Satellite observations of mesoscaleeddy dynamics in the eastern tropical Pacific Ocean. J. Phys.Oceanogr. 7: 648–658.Trasviña A, Barton ED. 2008. Summer circulation in the Mexicantropical Pacific. Deep-Sea Res. I 55: 587–607.Trasviña A, Barton ED, Brown J, Vélez HS, Kosro PM, Smith RL.1995. Offshore wind forcing in the Gulf of Tehuantepec,Mexico: The asymmetric circulation. J. Geophys. Res.100(C10): 20649–20663.Wyrtki K. 1965. Surface currents of the eastern tropical Pacificocean. Inter-Am. Trop. Tuna Comm. Bull. 9 (5): 271–304.Received December 2010;accepted May 2011.456