DMCA
1997b): Temporal and spatial variabilities of the South China Sea surface temperature anomaly
| Venue: | J. Geophys. Res |
| Citations: | 36 - 17 self |
Citations
| 956 |
Analysis of a complex of a statistical variables into principal components
- Hotelling
- 1933
(Show Context)
Citation Context ...(i = 1, 2, .., 21; j = 1,s2, ... 26). EOF analysis widely used in oceanographicsand meteorological research [e.g., Weare et al., 1976;sRichman, 1986] is the same as principal components(PC) analysis [=-=Hotelling, 1933-=-] in the statistics com-smunity. PCs are the amplitudes, which are functions ofstime, of their corresponding EOFs. These EOFs can besfound by calculating the unitary eigenvectors of the co-svariance m... |
| 654 |
M.: Improved global sea surface temperature analyses using optimum interpolation
- Reynolds, Smith
- 1994
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Citation Context ... of thesSouth China Sea.sThe SST data (1982-1994) for this study were ob-stained from the NCEP monthly real-time SST globalsdata set, which was established by blending in situsand satellite SST data [=-=Reynolds, 1988-=-; Reynolds andsMarsico, 1993]. The monthly optimum interpolations(OI) fields are derived from linear interpolation of thesweekly OI fields to daily fields then averaging the dailysvalues over a month ... |
| 173 |
Rotation of principal components.
- Richman
- 1986
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Citation Context ...ears of monthly data; N - 546scorresponds to the number of grids (i = 1, 2, .., 21; j = 1,s2, ... 26). EOF analysis widely used in oceanographicsand meteorological research [e.g., Weare et al., 1976;s=-=Richman, 1986-=-] is the same as principal components(PC) analysis [Hotelling, 1933] in the statistics com-smunity. PCs are the amplitudes, which are functions ofstime, of their corresponding EOFs. These EOFs can bes... |
| 67 | A Global Ocean Wind Stress Climatology Based - Trenberth, Olsen, et al. - 1989 |
| 31 | South China Sea warm pool detected in spring from - Tseng, P - 1997 |
| 15 | South China Sea warm Pool in boreal spring - Chu - 1997 |
| 12 | Oceanographic conditions in the sea east of Philippines and Luwn Strait in summer of 1965 and - Nitani - 1970 |
| 10 | Winds and drift currents in - Dale - 1956 |
| 2 | China Sea warm pool and monsoon development, paper presented at - Chu, Chang, et al. |
| 1 | A case study of the South China Sea warm anomaly, paper presented at - Chu, Chang |
| 1 |
South China Sea warm-core and cold-core ddies detected from the Navy's Master Oceanographic Observational Data Set
- Chu, Tseng, et al.
- 1996
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Citation Context ... quite well with the early study usingsanomaly exists in the SCS using the National Meteoro- the Navy's Master Oceanographic Observation Data Setslogical Center (.rr) monthly sea surface temperature [=-=Chu et al., 1996-=-, 1997].s20,954 CHU ET AL.: SOUTH CHINA SEA SURFACE TEMPERATURE VARIABILITIESs25s2OsZ15s10s25s2OsZ15s'•1os-/0..4so.6•s<-.-i7•s/s/ /s110 115 120 125sLongitude(E), Depth=O(m)sFigure 12. (continued)s110 ... |
| 1 | Improved global surface temperature analyses using optimum interpolation - Reynolds, Smith - 1994 |
| 1 |
Cold-core eddy detected in South China Sea. Eos Trans
- Soong, Hu, et al.
- 1995
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Citation Context ...ason [Chusand Chang, 1995a, b, 1997; Chuet al., 1996, 1997] andsa cool anomaly was detected in the central SCS duringsDecember 29, 1993 to January 5, 1994 from the analy-ssis of TOPEX/ POSEIDON data [=-=Soong et al., 1995-=-].sWhat are the temporal and spatial variabilities of seassurface temperature (SST) anomaly? We used the Na-stional Centers for Environmental Prediction (NCEP)sSST data set to investigate these proble... |
