Estimates of potential new production in the Java-Sumatra upwelling system

Xing Wei; Xiaomei Liao; Haigang Zhan; Hailong Liu

doi:10.1007/s00343-012-1281-x

Your Location：

Home >

Browse articles >

Estimates of potential new production in the Java-Sumatra upwelling system

OriginalPaper | Updated：2023-05-16

- Estimates of potential new production in the Java-Sumatra upwelling system
- Estimates of potential new production in the Java-Sumatra upwelling system
- 海洋湖沼学报（英文） 2012年30卷第6期页码：1063-1067
- Affiliations：
  
  1. State Key Laboratory of Tropical Oceanography South China Sea Institute of Oceanology Chinese Academy of Sciences
  2. State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics Institute of Atmospheric Physics Chinese Academy of Sciences
- Author bio：
- Funds：
  
  Supported by the Knowledge Innovation Program of Chinese Academy of Sciences (Nos. KZCX2-YW-Q11-02, LYQY200807) and the National Natural Science Foundation of China (No. 40876093)
- DOI：10.1007/s00343-012-1281-x
  中图分类号：
- 网络首发：2012-11-17，
  
  纸质出版：2012
- Accepted：
Scan QR Code
Estimates of potential new production in the Java-Sumatra upwelling system[J]. 海洋湖沼学报（英文）, 2012,30(6):1063-1067.

Wei, X., Liao, X., Zhan, H. et al. Estimates of potential new production in the Java-Sumatra upwelling system., Chin. J. Ocean. Limnol. 30, 1063–1067 (2012). https://doi.org/10.1007/s00343-012-1281-x
Estimates of potential new production in the Java-Sumatra upwelling system[J]. 海洋湖沼学报（英文）, 2012,30(6):1063-1067. DOI： 10.1007/s00343-012-1281-x.

Wei, X., Liao, X., Zhan, H. et al. Estimates of potential new production in the Java-Sumatra upwelling system., Chin. J. Ocean. Limnol. 30, 1063–1067 (2012). https://doi.org/10.1007/s00343-012-1281-x DOI：

摘要

Abstract

The Java-Sumatra upwelling is one of the most important upwelling systems in the Indian Ocean

with maximum upwelling intensity in July through August. To estimate the nitrate supplied by upwelling

we developed a three-dimensional hydrodynamic model to calculate the mean vertical speed and determine the depth of upwelling. We used in-situ vertical nitrate profiles to assess nitrate concentration in the upwelled waters

and calculated the nitrate supply as the product of nitrate concentration and vertical transport obtained from the numerical model. The calculated result represents potential new production generated in the upwelling region. We found that on the event time scale (monthly) of Java-Sumatra upwelling

water brought to the surface originated from locations 100-m deep

giving a nitrate supply of 93.77×103 mol/s and potential new production of 1.02×1014 gC/a.

关键词

Keywords

references

Bakun A. 1973. Coastal upwelling indices, west coast of North America, 1946–1971. NOAA Tech. Rep. NMFS SSFR-671. p.103.

Boyer T P, Antonov J I, Baranova O K, Garcia H E, Johnson D R, Locarnini R A, Mishonov A V, O’Brien T D, Seidov D, Smolyar I V, Zweng M M. 2009. World Ocean Database 2009. In: Levitus S ed. NOAA Atlas NESDIS 66, US. Gov. Printing Office, Wash. DC. p.216.

Boyer T P, Levitus S, Antonov J, Conkright M, O’Brien T, Stephens C. 1998. World Ocean Atlas 1998 Vol. 4: Salinity of the Atlantic Ocean. NOAA Atlas NESDIS 30, US. Gov. Printing Offi ce, Wash. DC.

Brink K H, Abrantes F F G, Bernal P A, Dugdale R C, Estrada M, Hutchings L, Jahnke R A, Muller P J, Smith R L. 1995. How do coastal upwelling systems operate as integrated physical, chemical, and biological systems and infl uence the geological record? The role of physical processes in defi ning the spatial structures of biological and chemical variables. In: Summerhayes C P, Emeis K C, Angel M V, Smith R L, Zeitzschel B eds. Upwelling in the Ocean: Modern Processes and Ancient Records. Wiley, Chichester, UK. p.103–124.

Canuto V M, Howard A, Cheng Y, Dubovikov M S. 2001. Ocean turbulence. Part I: one-point closure modelmomentum and heat vertical diffusivities. J. Phys. Oceanog., 31: 1 413–1 426.

Carmack E C, Aagaard K. 1977. A note on volumetric considerations of upwelling in the Benguela Current. Estuar. Coast. Mar. Sci., 5: 135–142.

Carton J A, Giese B S. 2008. A reanalysis of ocean climate using simple ocean data assimilation (SODA). Mon. Weather Rev., 136(8): 2 999, http://dx.doi.org/10.1175/2007MWR1978.1.

Chavez F P, Barber R T. 1987. An estimate of new production in the equatorial Pacifi c. Deep-Sea Res. I, 34 (7): 1 229–1 243.

Chavez F P, Barber R T, Sanderson M P. 1989. The potential primary production of the Peruvian upwelling ecosystem, 1953–1984. In: Pauly D, Muck P, Mendo J, Tsukayama I eds. The Peruvian Upwelling Ecosystem: Dynamics and Interactions. ICLARM Conference Proceedings. p.50–63.

Chavez F P, Toggweiler J R. 1995. Physical estimates of global new production: the upwelling contribution. In: Summerhayes C P, Emeis K C, Angel M V, Smith R L, Zeitzschel B eds. Upwelling in the Ocean: Modern Processes and Ancient Records. Wiley, Chichester, UK. p.313–320.

Chavez F P, Messié M. 2009. A comparison of eastern boundary upwelling ecosystems. Prog. Oceanogr., 83: 80–96.

Du Y, Qu T, Meyers G, Masumoto Y, Sasaki H. 2005. Seasonal heat budget in the mixed layer of the southeastern tropical Indian Ocean in a high-resolution ocean general circulation model. J. Geophys. Res., 110: C04012, http://dx.doi.org/10.1029/2004JC002845.

Dugdale R C, Goering J J. 1967. Uptake of new and regenerated nitrogen in primary productivity. Limnol. Oceanog., 12: 196–206.

Gent P R, McWilliams J C. 1990. Isopycnal mixing in ocean circulation models. J. Phys. Oceanogr., 20: 150–155.

Griffies S M, Biastoch A, Böning C, Bryan F, Danabasoglu G, Chassignet E P, England M E, Gerdes R, Haak H, Hallberg R W, Hazeleger W, Jungclaus J, Large W G, Madec G, Pirani A, Samuels B L, Scheinert M, Sen Gupta A, Severijns C A, Simmons H L, Treguier A M, Winton M, Yeager S, Yin J. 2009. Coordinated Ocean-ice Reference Experiments (COREs). Ocean Model., 26: 1–46.

Kamykowski D. 1987. A preliminary biophysical model of the relationship between temperature and plant nutrients in the upper ocean. Deep-Sea Res., 34: 1 067–1 079.

Large W, Yeager S. 2004. Diurnal to Decadal Global Forcing for ocean and Sea-Ice Models: the Data Sets and Flux Climatologies. NCAR/TN-460+STR, Colorado.

Liu H L, Yu Y Q, Li W, Zhang H. 2004. Manual for LASG/IAP Climate System Ocean Model (LICOM1.0). Science Press, Beijing, China. p.1–105. (in Chinese)

Mendo J, Bohle-Carbonell M, Calienes R, 1989. Time series of upwelling nitrate and primary production off Peru derived from wind and ancillary data, 1953–1982. In: Pauly D, Muck P, Mendo J, Tsukayama I eds. The Peruvian Upwelling Ecosystem: Dynamics and Interactions. ICLARM Conference Proceedings. p.64–77.

Messié M, Ledesma J, Kolber D D, Michisaki R P, Foley D G. 2009. Potential new production estimates in four eastern boundary upwelling ecosystems. Prog. Oceanogr., 83: 151–158.

Minas H J, Minas M, Packard T T. 1986. Productivity in upwelling areas deduced from hydrographic and chemical fi elds. Limnol. Oceanogr., 31 (6): 1 182–1 206.

Mo H E, Yu Y Q, Liu H L, Lin P F. 2009. Preliminary results from a high-resolution Pacifi c-Indian basin-wide ocean general circulation model general circulation model. J. Trop. Oceangr., 28(5): 56–65. (in Chinese)

Oschlies A, Garçon V. 1998. Eddy-induced enhancement of primary production in a model of the North Atlantic Ocean. Nature, 394: 263–269.

Silió-Calzada A, Bricaud A, Gentilli B. 2008. Estimates of sea surface nitrate concentrations from sea surface temperature and chlorophyll concentration in upwelling areas: a case study for the Benguela System. Remote Sens. Environ., 112: 3 173–3 180.

Stoens A, Menkes C, Radenac M H, Dandonneau Y, Grima N, Eldin G et al. 1999. The coupled physical new production system in the equatorial Pacifi c during the 1992–1995 El Niño. J. Geophys. Res., 104: 3 323–3 339.

Susanto R D, Gordon A L, Zheng Q. 2001. Upwelling along the coasts of Java and Sumatra and its relation to ENSO. Geophy. Res. Lett., 28 (8): 1 599–1 602.

Valsala V, Maksyutov S. 2010. A short surface pathway of the subsurface Indonesian throughfl ow water from the Java coast associated with upwelling, Ekman transport, and subduction. Int. J. Oceanogr., 2010, http://dx.doi.org/10.1155/2010/540783

Walsh J J. 1991. Importance of continental margins in the marine biogeochemical cycling of carbon and nitrogen. Nature, 350: 53–55.

浏览量

Downloads

CSCD

文章被引用时，请邮件提醒。

Submit

工具集

关联资源

暂无数据