跳至主要内容

The Influence of Large-Scale Phenomena on La Paz Bay Hydrographic Variability

Read  full  paper  at:
http://www.scirp.org/journal/PaperInformation.aspx?PaperID=53548#.VMiF7izQrzE

ABSTRACT
We analyzed the hydrographic variability of La Paz Bay, the largest coastal water body in the Gulf of California, and its relationship to Pacific large-scale phenomena, including the El Ni?o-Southern Oscillation (ENSO), Pacific Decadal Oscillation (PDO), Pacific-North America pattern (PNA), and North Pacific pattern (NP). We used several indices related to these phenomena and the hydrographic variability data of La Paz Bay, consisting of the annual sea surface temperature patterns from satellite imagery from 2000 to 2010 and the mixed layer depths measured with in situ data from 1994 to 2009. The results indicate the sea surface temperature fluctuated during the study period, with 2007 as the coldest year and 2009 as the warmest. Two periods were identified in the annual thermal cycle of the bay, one period of warmth from June to November, and one of cold from December to May. The sea surface temperature is primarily influenced by the ENSO. The mixed layer depth analysis showed its absence during August-September, while the deepest ones were in November-March. The unusual 100 m mixed layer depth noted during February 2002 and its absence in March 1996 and 2009 were related to uncommon atmospheric conditions in the annual patterns of the ENSO, PNA, and NP. The variability of the mixed layer depth is primarily related to the variability of the NP. We concluded that the hydrographic conditions of La Paz Bay are most influenced by the NP during the cold phase of its annual cycle, and by the ENSO during the warm phase.
 
Cite this paper
Guevara-Guillén, C. , Shirasago-Germán, B. and Pérez-Lezama, E. (2015) The Influence of Large-Scale Phenomena on La Paz Bay Hydrographic Variability. Open Journal of Marine Science, 5, 146-157. doi: 10.4236/ojms.2015.51012.
 
References
[1]Schwing, F.B., Murphree, T. and Green, P.M. (2002) The Northern Oscillation Index (NOI): A New Climate Index for the Northeast Pacific. Progress in Oceanography, 53, 115-139.
http://dx.doi.org/10.1016/S0079-6611(02)00027-7
 
[2]Parrish, R.H., Schwing, F.B. and Mendelssohn, R. (2000) Mid-Latitude Wind Stress: The Energy Source for Climate Shifts in the North Pacific Ocean. Fisheries Oceanography, 9, 224-238.
http://dx.doi.org/10.1046/j.1365-2419.2000.00136.x
 
[3]Wooster, W.S. and Hollowed, A.B. (1995) Decadal-Scale Variations in the Eastern Subarctic Pacific, 1: Winter Ocean Conditions. Canadian Special Publication of Fisheries and Aquatic Sciences, 121, 81-85.
 
[4]Bograd, S.J., Chereskin, T.K. and Roemmich, D. (2001) Transport of Mass, Heat, Salt, and Nutrients in the Southern California Current System: Annual Cycle and Interannual Variability. Journal of Geophysical Research, 106, 9255-9275. http://dx.doi.org/10.1029/1999JC000165
 
[5]Bernal, P.A. and Chelton, D.B. (1984) Variabilidad biológica de baja frecuencia y gran escala en la Corriente de California, 1949-1978 (Low Frequency and Large-Scale Biological Variability in the California Current, 1949-1978). In: Csirke, J. and Sharp, G.D., Eds., Reports of the Expert Consultation to Examine Changes in Abundance and Species Composition of Neritic Fish Resources. San José, Costa Rica, 18-29. A Preparatory Meeting for the FAO World Conference on Fisheries Management and Development. FAO Fisheries Report, 1, 102 p.
 
[6]Schwing, F.B., Murphree, T., deWitt, L. and Green, P.M. (2002) The Evolution of Oceanic and Atmospheric Anomalies in the Northeast Pacific during the El Nino and La Nina Events of 1995-2001. Progress in Oceanography, 54, 459-491. http://dx.doi.org/10.1016/S0079-6611(02)00064-2
 
[7]Deser, C., Alexander, M.A. and Timlin, M.S. (1999) Evidence for a Wind-Driven Intensification of the Kuroshio Current Extension from the 1970s to the 1980s. Journal of Climate, 12, 1697-1706.
http://dx.doi.org/10.1175/1520-0442(1999)012<1697:EFAWDI>2.0.CO;2
 
[8]Barlow, M., Nigam, S. and Berbery, E.H. (2001) ENSO, Pacific Decadal Variability, and US Summertime Precipitation, Drought, and Stream Flow. Journal of Climate, 14, 2105-2128.
http://dx.doi.org/10.1175/1520-0442(2001)014<2105:EPDVAU>2.0.CO;2
 
[9]Herrera-Cervantes, H., Lluch-Cota, D.B., Lluch-Cota, S.E. and Gutiérrez de Velasco, G. (2007) The ENSO Signature in Sea-Surface Temperature in the Gulf of California. Journal of Marine Research, 65, 589-605.
http://dx.doi.org/10.1357/002224007783649529
 
[10]Chiew, F.H. and McMahon, T.A. (2002) Global ENSO-Streamflow Teleconnection, Streamflow Forecasting and Interannual Variability. Hydrological Sciences Journal, 47, 505-522.
http://dx.doi.org/10.1080/02626660209492950
 
[11]Trenberth, K.E. (1997) The Definition of El Ni?o. Bulletin of the American Meteorological Society, 78, 2771-2777. http://dx.doi.org/10.1175/1520-0477(1997)078<2771:TDOENO>2.0.CO;2
 
[12]Mantua, N.J., Hare, S.R., Zhang, Y., Wallace, J.M. and Francis, R.C. (1997) A Pacific Interdecadal Climate Oscillation with Impacts on Salmon Production. Bulletin of the American Meteorological Society, 78, 1069-1079. http://dx.doi.org/10.1175/1520-0477(1997)078<1069:APICOW>2.0.CO;2
 
[13]Mantua, N.J. and Hare, S.R. (2002) The Pacific Decadal Oscillation. Journal of Oceanography, 58, 35-44. http://dx.doi.org/10.1023/A:1015820616384
 
[14]Mantua, N.J. (1999) The Pacific Decadal Oscillation and Climate Forecasting for North America. Joint Institute for the Study of the Atmosphere and Oceans, University of Washington, Seattle.
http://www.atmos.washington.edu/~mantua/REPORTS/PDO/PDO_cs.htm
 
[15]Piechota, T.C., Garbrecht, J.D. and Schneider, J.M. (2006) Climate Variability and Climate Change. In: Garbrecht, J.D. and Piechota, T.C., Eds., Climate Variations, Climate Change, and Water Resources Engineering, ASCE, Reston, VA, 1-18.
 
[16]Wallace, J.M. and Gutzler, D.S. (1981) Teleconnections in the Geopotential Height Field during the Northern Hemisphere Winter. Monthly Weather Review, 109, 784-812.
http://dx.doi.org/10.1175/1520-0493(1981)109<0784:TITGHF>2.0.CO;2
 
[17]Wallace, J.M. (2000) North Atlantic Oscillation/Annular Mode: Two Paradigms-One Phenomenon. Quarterly Journal of the Royal Meteorological Society, 126, 791-805.
http://dx.doi.org/10.1256/smsqj.56401
 
[18]Blackmon, M.L., Lee, Y.-H. and Wallace, J. (1984) Horizontal Structure of 500 mb Height Fluctuations with Long, Intermediate and Short Time Scales. Journal of the Atmospheric Sciences, 41, 961-979. http://dx.doi.org/10.1175/1520-0469(1984)041<0961:HSOMHF>2.0.CO;2
 
[19]Blackmon, M.L., Lee, Y.-H., Wallace, J. and Hsu, H.-H. (1984) Time Variation of 500 mb Height Fluctuations with Long, Intermediate and Short Time Scales as Deduced from Lag-Correlation Statistics. Journal of the Atmospheric Sciences, 41, 981-991.
http://dx.doi.org/10.1175/1520-0469(1984)041<0981:TVOMHF>2.0.CO;2
 
[20]Trenberth, K.E., Branstator, G.W., Karoly, D., Kumar, A., Lau, N. and Ropelewski, C. (1998) Progress during TOGA in Understanding and Modeling Global Teleconnections Associated with Tropical Sea Surface Temperature. Journal of Geophysical Research, 103, 14291-14324. http://dx.doi.org/10.1029/97JC01444
 
[21]Straus, D.M. and Shukla, J. (2002) Does ENSO Force the PNA? Journal of Climate, 15, 2340-2358.
http://dx.doi.org/10.1175/1520-0442(2002)015<2340:DEFTP>2.0.CO;2
 
[22]Lin, J.L., Zhang, M.H. and Mapes, B.E. (2005) Zonal Momentum Budget of the Madden-Julian Oscillation: The Source and Strength of Equivalent Linear Damping. Journal of the Atmospheric Sciences, 62, 2172-2188. http://dx.doi.org/10.1175/JAS3471.1
 
[23]Trenberth, K.E. and Hurrell, J.W. (1994) Decadal Atmospheric-Ocean Variations in the Pacific. Climate Dynamics, 9, 303-319. http://dx.doi.org/10.1007/BF00204745
 
[24]Lavín, M.F., Beier, E. and Badan, A. (1997) Estructura hidrográfica y circulación del Golfo de California: Escalas estacional e interanual. In: Lavín, M.F., Ed., Contribuciones a la Oceanografía Física en México, Unión Geofísica Mexicana, Monografía No. 3, 141-171.
 
[25]Makarov, V.G. and Jiménez-Illescas, A.R. (2003) Barotropic Background Currents in the Gulf of California. Ciencias Marinas, 29, 141-153.
 
[26]Marinone, S.G. (2003) A Three Dimensional Model of the Mean and Seasonal Circulation of the Gulf of California. Journal of Geophysical Research, 108, 3325. http://dx.doi.org/10.1029/2002JC001720
 
[27]Soto-Mardones, L., Marinone, S.G. and Parés-Sierra, A. (1999) Time and Spatial Variability of Sea Surface Temperature in the Gulf of California. Ciencias Marinas, 25, 1-30.
 
[28]Lavín, M.F., Palacios-Hernández, E. and Cabrera, C. (2003) Sea Surface Temperature Anomalies in the Gulf of California. Geofísica Internacional, 42, 363-375.
 
[29]Latif, M. and Barnett, T.P. (1995) Interactions of the Tropical Oceans. Journal of Climate, 8, 952-964. http://dx.doi.org/10.1175/1520-0442(1995)008<0952:IOTTO>2.0.CO;2
 
[30]Zhang, Y., Wallace, J.M. and Battisti, D.S. (1997) ENSO-Like Interdecadal Variability: 1900-93. Journal of Climate, 10, 1004-1020. http://dx.doi.org/10.1175/1520-0442(1997)010<1004:ELIV>2.0.CO;2
 
[31]Hare, S. and Mantua, N. (2000) Empirical Evidence for North Pacific Regime Shifts in 1977 and 1989. Progress in Oceanography, 47, 103-145. http://dx.doi.org/10.1016/S0079-6611(00)00033-1
 
[32]Martinez, E., Antoine, D., D’Ortenzio, F. and Gentili, B. (2009) Climate-Driven Basin-Scale Decadal Oscillations of Oceanic Phytoplankton. Science, 326, 1253-1256.
http://dx.doi.org/10.1126/science.1177012
 
[33]Di Lorenzo, E., Schneider, N., Cobb, K.M., Chhak, K., Franks, P.J.S., Miller, A.J., McWilliams, J.C., Bograd, S.J., Arango, H., Curchister, E., Powell, T.M. and Rivere, P. (2008) North Pacific Gyre Oscillation Links Ocean Climate and Ecosystem Change. Geophysical Research Letters, 35, Article ID: L08607.
http://dx.doi.org/10.1029/2007GL032838
 
[34]Horel, J.D. and Wallace, J.M. (1981) Planetary-Scale Atmospheric Phenomena Associated with the Southern Oscillation. Monthly Weather Review, 109, 2080-2092.
http://dx.doi.org/10.1175/1520-0493(1981)109<2080:ARPCAO>2.0.CO;2
 
[35]Namias, J. and Cayan, D.R. (1981) Large-Scale Air-Sea Interactions and Short Period Climate Fluctuations. Science, 214, 869-876. http://dx.doi.org/10.1126/science.214.4523.869
 
[36]Wallace, J.M. and Jiang, Q. (1987) On the Observed Structure of the Interannual Variability of the Atmosphere-Ocean Climate System. In: Cattle, H., Ed., Atmospheric and Oceanic Variability, Royal Meteorological Society, Bracknell, 17-43.
 
[37]Hoskins, B.J. and Karoly, D.J. (1981) The Steady Linear Response of a Spherical Atmosphere to Thermal and Orographic Forcing. Journal of the Atmospheric Sciences, 38, 1179-1196.
http://dx.doi.org/10.1175/1520-0469(1981)038<1179:TSLROA>2.0.CO;2
 
[38]Wallace, J.M., Smith, C. and Bretherton, C.S. (1992) Singular Value Decomposition of Wintertime Sea Surface Temperature and 500 mb Height Anomalies. Journal of Climate, 5, 561-576.
http://dx.doi.org/10.1175/1520-0442(1992)005<0561:SVDOWS>2.0.CO;2
 
[39]Limsakul, A., Saino, T., Midorikawa, T. and Goes, J.I. (2001) Temporal Variations in Lower Trophic Level Biological Environments in the Northwestern North Pacific Subtropical Gyre from 1950 to 1997. Progress in Oceanography, 49, 129-149. http://dx.doi.org/10.1016/S0079-6611(01)00019-2
 
[40]Jerónimo, G. and Gómez-Valdés, J. (2010) Mixed Layer Depth Variability in the Tropical Boundary of the California Current, 1997-2007. Journal of Geophysical Research, 115, Article ID: C05014.
http://dx.doi.org/10.1029/2009JC005457
 
[41]Obeso-Nieblas, M., Shirasago-Germán, B., Gavi?o-Rodríguez, J.H., Pérez-Lezama, E.L., Obeso-Huerta, H. and Jiménez-Illescas, A.R. (2008) Variabilidad hidrográfica en Bahía de La Paz, Golfo de California, México (1995-2005). Revista de Biología Marina y Oceanografía, 43, 559-567. http://dx.doi.org/10.4067/S0718-19572008000300015
 
[42]Obeso-Nieblas, M. (2003) Variabilidad espaciotemporal de las condiciones oceanográficas de la Bahía de La Paz, BCS, México. Ph.D. Dissertation, Centro Interdisciplinario de Ciencias Marinas, Instituto Politécnico Nacional, Mexico City.
 
[43]Guevara-Guillén, C. (2011) Hidrografía en Bahía de La Paz y zona oceánica adyacente. Masters Dissertation, Centro Interdisciplinario de Ciencias Marinas, Instituto Politécnico Nacional, Mexico City.
 
[44]Cruz Orozco, R., Martínez-Noriega, C. and Mendoza-Maravillas, A. (1996) Batimetría y sedimentos en la Bahía de La Paz. Oceánides, 7, 21-27.
 
[45]Salinas-González, F., Zaytsev, O. and Makarov, V.G. (2003) Formación de estructura termohalina del agua en la Bahía de La Paz de verano a oto?o. Ciencias Marinas, 29, 51-65.
 
[46]Sánchez-Velasco, L., Beier, E., Avalos-Garcia, C. and Lavín, M.F. (2006) Larval Fish Assemblages and Geostrophic Circulation in Bahia de La Paz and the Surrounding Southwestern Region of the Gulf of California. Journal of Plankton Research, 28, 1-18. http://dx.doi.org/10.1093/plankt/fbl040
 
[47]Zaytsev, O., Rabinovich, A.B., Thomson, R.E. and Silverberg, N. (2010) Intense Diurnal Surface Currents in the Bay of La Paz, Mexico. Continental Shelf Research, 30, 608-619.
http://dx.doi.org/10.1016/j.csr.2009.05.003
 
[48]Obeso-Nieblas, M., Shirasago-Germán, B., Sánchez-Velasco, L. and Gavi?o-Rodríguez, J.H. (2004) Hydrographic Variability in Bahía de La Paz, BCS, México, during the 1997-1998 El Ni?o. Deep Sea Research Part II, 51, 689-710. http://dx.doi.org/10.1016/j.dsr2.2004.05.005
 
[49]Kahru, M. (2014) Windows Image Manager, WIM Software (Ver. 7.05) and User’s Manual, 125 p. http://www.wimsoft.com/
 
[50]Climate Prediction Center Internet Team (2005) Oceanic Ni?o Index (ONI), Multivariate ENSO Index (MEI), Bivariate ENSO Timeseries (BEST), Southern Oscillation Index (SOI), Northern Oscillation Index (NOI), Pacific Decadal Oscillation (PDO), Pacific North American index (PNA) and North Pacific Pattern Index (NP) (Online). NOAA/National Weather Service, National Centers for Environmental Prediction, Climate Prediction Center. http://www.esrl.noaa.gov/psd/data/climateindices/list/
 
[51]Castro, R., Mascare?as, A.S., Durazo, R. and Collins, C.A. (2000) Seasonal Variation of the Temperature and Salinity at the Entrance to the Gulf of California, México. Ciencias Marinas, 26, 561-583.
 
[52]Sánchez-Velasco, L., Valdéz-Holguín, J.E., Shirasago-Germán, B., Cisneros-Mata, M.A. and Zárate, A. (2002) Changes in the Spawning Environment of Sardinops caeruleus in the Gulf of California during El Nino 1997-1998. Estuarine Coastal and Shelf Science, 54, 207-217.
http://dx.doi.org/10.1006/ecss.2001.0840
 
[53]Pacheco-Ruíz, I., Becerril-Bobadilla, F., Zertuche-González, J.A., Barragán, A.C., Gálvez-Telles, A. and Blanco-Betancourt, R. (2003) Effects of El Ni?o on Beds of Ulva lactuca along the Northwest Coast of the Gulf of California, Mexico. Geofísica Internacional, 42, 447-454.
 
[54]Douglas, M.W., Maddox, R.A., Howard, K. and Reyes, S. (1993) The Mexican Monsoon. Journal of Climate, 6, 1665-1678. http://dx.doi.org/10.1175/1520-0442(1993)006<1665:TMM>2.0.CO;2            eww150128lx

评论

此博客中的热门博文

Does Immigration Promote the Investment of the Monopolistic Firm?

In the present paper, we examine the effect of increasing uncertainty of immigrants’ growth on the optimal timing of investment of a firm that has a monopolistic power over the labor market. It is revealed that when the uncertainty of immigrants’ growth is more than a threshold level, increasing uncertainty of immigrants’ growth accelerates the optimal timing of firms’ investment and enhances the economic growth, even if the uncertainty of immigrants’ growth is formulated by the geometric Brownian motion, which is in sharp contrast to the standard result that an increase in the uncertainty postpones the optimal timing. With an increase in the immigrants over the past ten years, workforces in the host countries have been growing significantly to the extent that the immigrants represent 70% of the increase in the workforce in Europe, and 47% in the United States as OECD indicates. In the present paper, we attempted to investigate the effect of increased uncertainty caused by the growi...

Education Policy Implementation: A Mechanism for Enhancing Primary Education Development in Zanzibar

Education is one of the fundamental rights of individuals; therefore, the government of a country needs to develop and strengthen educational policy and quality as well as to ensure that everyone has equal access to basic education. The improvement of access and quality of education in the world is becoming as an essential factor in development, whereas the basic education (primary school), is acknowledged as a foundation of the higher educational development for every country. To fulfill this goal, governments introduce several policies and procedures; however, it requires some reforms and participation from the politician, policymakers, and other stakeholders to re-examine educational policy so that it can lead to multiplication and betterment of the reforms. Educational reforms actually focus on accountability. A positive educational development and reform is very challenging and needs more effort and strategy on how to use and utilize the resources effectively as such it can achie...