Abstract
The northward migration of spring bloom was observed in the Sea of Japan from April to May 1997 by the Ocean Color and Temperature Scanner (OCTS) on board the Advanced Earth Observing Satellite (ADEOS). This phenomenon is well simulated with a numerical ecosystem model coupled with a hydrodynamic model. The hydrodynamic model is the Geophysical Fluid Dynamics Laboratory (GFDL) Modular Ocean Model (MOM). The ecosystem model consists of five components: dissolved inorganic nitrogen (DIN), dissolved inorganic phosphorus (DIP), phytoplankton, zooplankton and detritus. Results of the numerical ecosystem model suggest that the mesoscale development of the spring bloom in the Sea of Japan is related to that of sea water temperature, and that the bloom is limited by the depletion of DIN.
| Original language | English |
|---|---|
| Pages (from-to) | 617-630 |
| Number of pages | 14 |
| Journal | Journal of Oceanography |
| Volume | 57 |
| Issue number | 6 |
| DOIs | |
| Publication status | Published - Dec 1 2001 |
Fingerprint
All Science Journal Classification (ASJC) codes
- Oceanography
Cite this
A numerical simulation on the Mesoscale dynamics of the spring bloom in the sea of Japan. / Yanagi, Tetsuo; Onitsuka, Goh; Hirose, Naoki; Yoon, John Hwan.
In: Journal of Oceanography, Vol. 57, No. 6, 01.12.2001, p. 617-630.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - A numerical simulation on the Mesoscale dynamics of the spring bloom in the sea of Japan
AU - Yanagi, Tetsuo
AU - Onitsuka, Goh
AU - Hirose, Naoki
AU - Yoon, John Hwan
PY - 2001/12/1
Y1 - 2001/12/1
N2 - The northward migration of spring bloom was observed in the Sea of Japan from April to May 1997 by the Ocean Color and Temperature Scanner (OCTS) on board the Advanced Earth Observing Satellite (ADEOS). This phenomenon is well simulated with a numerical ecosystem model coupled with a hydrodynamic model. The hydrodynamic model is the Geophysical Fluid Dynamics Laboratory (GFDL) Modular Ocean Model (MOM). The ecosystem model consists of five components: dissolved inorganic nitrogen (DIN), dissolved inorganic phosphorus (DIP), phytoplankton, zooplankton and detritus. Results of the numerical ecosystem model suggest that the mesoscale development of the spring bloom in the Sea of Japan is related to that of sea water temperature, and that the bloom is limited by the depletion of DIN.
AB - The northward migration of spring bloom was observed in the Sea of Japan from April to May 1997 by the Ocean Color and Temperature Scanner (OCTS) on board the Advanced Earth Observing Satellite (ADEOS). This phenomenon is well simulated with a numerical ecosystem model coupled with a hydrodynamic model. The hydrodynamic model is the Geophysical Fluid Dynamics Laboratory (GFDL) Modular Ocean Model (MOM). The ecosystem model consists of five components: dissolved inorganic nitrogen (DIN), dissolved inorganic phosphorus (DIP), phytoplankton, zooplankton and detritus. Results of the numerical ecosystem model suggest that the mesoscale development of the spring bloom in the Sea of Japan is related to that of sea water temperature, and that the bloom is limited by the depletion of DIN.
UR - http://www.scopus.com/inward/record.url?scp=0035694827&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0035694827&partnerID=8YFLogxK
U2 - 10.1023/A:1021691221793
DO - 10.1023/A:1021691221793
M3 - Article
VL - 57
SP - 617
EP - 630
JO - Journal of Oceanography
JF - Journal of Oceanography
SN - 0916-8370
IS - 6
ER -