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Parés-Sierra, A., Mascarenhas, A., Marinone, S. G., Castro, R. (2003) Temporal and spatial variation of the surface winds in the Gulf of California. Geophysical Research Letters, 30 (6) doi:10.1029/2002gl016716

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Reference TypeJournal (article/letter/editorial)
TitleTemporal and spatial variation of the surface winds in the Gulf of California
JournalGeophysical Research Letters
AuthorsParés-Sierra, A.Author
Mascarenhas, A.Author
Marinone, S. G.Author
Castro, R.Author
Year2003 (March)Volume30
Issue6
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/2002gl016716Search in ResearchGate
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Mindat Ref. ID809442Long-form Identifiermindat:1:5:809442:5
GUID0
Full ReferenceParés-Sierra, A., Mascarenhas, A., Marinone, S. G., Castro, R. (2003) Temporal and spatial variation of the surface winds in the Gulf of California. Geophysical Research Letters, 30 (6) doi:10.1029/2002gl016716
Plain TextParés-Sierra, A., Mascarenhas, A., Marinone, S. G., Castro, R. (2003) Temporal and spatial variation of the surface winds in the Gulf of California. Geophysical Research Letters, 30 (6) doi:10.1029/2002gl016716
In(2003, March) Geophysical Research Letters Vol. 30 (6) American Geophysical Union (AGU)

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Marinone, S. G., Parés-Sierra, A., Castro, R., Mascarenhas, A. (2004) Correction to “Temporal and Spatial variation of the surface winds in the Gulf of California”. Geophysical Research Letters, 31 (10) doi:10.1029/2004gl020064
Marinone, S. G. (2003) A three-dimensional model of the mean and seasonal circulation of the Gulf of California. Journal of Geophysical Research, 108. doi:10.1029/2002jc001720
Marinone, S. G. (2007) A note on “Why does the Ballenas Channel have the coldest SST in the Gulf of California?”. Geophysical Research Letters, 34 (2) doi:10.1029/2006gl028589
Mascarenhas, A. S. (2004) Seasonal variation of geostrophic velocity and heat flux at the entrance to the Gulf of California, Mexico. Journal of Geophysical Research, 109. doi:10.1029/2003jc002124
Marinone, S.G., Lavín, M.F., Parés-Sierra, A. (2011) A quantitative characterization of the seasonal Lagrangian circulation of the Gulf of California from a three-dimensional numerical model. Continental Shelf Research, 31 (14) 1420-1426 doi:10.1016/j.csr.2011.05.014
Marinone, S.G., Gutiérrez, O.Q., Parés-Sierra, A. (2004) Numerical simulation of larval shrimp dispersion in the Northern Region of the Gulf of California. Estuarine, Coastal and Shelf Science, 60. 611-617 doi:10.1016/j.ecss.2004.03.002
Marinone, S. G. (1998) Effect of the topographic stress on the tide- and wind-induced residual currents in the Gulf of California. Journal of Geophysical Research: Oceans, 103. 18437-18446 doi:10.1029/98jc01451
Marinone, S. G. (1997) Tidal residual currents in the Gulf of California: Is the M2tidal constituent sufficient to induce them?. Journal of Geophysical Research: Oceans, 102. 8611-8623 doi:10.1029/96jc03835
Beltrami, Hugo, Gosselin, C., Mareschal, J. C. (2003) Ground surface temperatures in Canada: Spatial and temporal variability. Geophysical Research Letters, 30 (10) doi:10.1029/2003gl017144
Collins, Curtis A., Garfield, Newell, Mascarenhas, Affonso S., Spearman, Monty G., Rago, Thomas A. (1997) Ocean currents across the entrance to the Gulf of California. Journal of Geophysical Research: Oceans, 102. 20927-20936 doi:10.1029/97jc01302
Chouet, Bernard (1979) Temporal variation in the attenuation of earthquake coda near Stone Canyon, California. Geophysical Research Letters, 6 (3) 143-146 doi:10.1029/gl006i003p00143
 
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