排序方式: 共有24条查询结果,搜索用时 546 毫秒
21.
Masafumi Kamachi Tsurane Kuragano Noriya Yoshiok Jiang Zhu Francesco Uboldi 《大气科学进展》2001,18(5):767-786
l. IntroductionLinear dynamics ls domlnant as a response to atmospheric forcing in the equatrialregion. In the mid-- to high--latitudes, ocean represents nonlinear phenomena such as strongcurrents and meso--scale eddies. Heat and water fluxes are also important. The resultantscales of the phenomena are rather small. We developed, for the mid-- to high--latitudes, anocean data assimilation system COMPASS--K: Comprehensive Ocean ModeIing, Prediction,Analysis and Synthesis System in the K… 相似文献
22.
Toyoda Takahiro Fujii Yosuke Kuragano Tsurane Kosugi Naohiro Sasano Daisuke Kamachi Masafumi Ishikawa Yoichi Masuda Shuhei Sato Kanako Awaji Toshiyuki Hernandez Fabrice Ferry Nicolas Guinehut Stéphanie Martin Matthew Andrew Peterson K. Good Simon A. Valdivieso Maria Haines Keith Storto Andrea Masina Simona Köhl Armin Yin Yonghong Shi Li Alves Oscar Smith Gregory Chang You-Soon Vernieres Guillaume Wang Xiaochun Forget Gael Heimbach Patrick Wang Ou Fukumori Ichiro Lee Tong Zuo Hao Balmaseda Magdalena 《Climate Dynamics》2017,49(3):891-907
Climate Dynamics - The interannual-decadal variability of the wintertime mixed layer depths (MLDs) over the North Pacific is investigated from an empirical orthogonal function (EOF) analysis of an... 相似文献
23.
Sea surface height anomaly maps of realistic eddy activity were obtained by applying space-time optimum interpolation to altimeter
data. Analysis error and rate of reconstructing eddy signals were investigated by taking account of: 1) dependency on orbit
configurations of single and multiple altimeters; 2) dependency on space-time scales of realistic, dominant eddies; and 3)
effect of space-time scales of eddy propagation. Large-scale sea surface height anomalies are subtracted from altimeter data
by applying an along-track filter to allow easy handling of eddy signals. The space-time scales of the first-guess error in
the optimum interpolation are statistically evaluated by fitting a space-time anisotropic Gaussian function to space-time-distributed
correlation coefficients of sea surface height using the TOPEX data. The results of the optimum interpolation clarify the
followings: 1) ERS has a better capability of reconstructing eddy signals than TOPEX. Comparison of maps from multi-altimeter
data shows that TOPEX+ERS has a better capability than Jason−1+TOPEX in lower latitudes and vice versa in higher latitudes,
though the differences are small. 2) The small space-time scale yields a low reconstruction rate in marginal seas and alongside
the equator. The persistent timescale is large, and westward propagation is dominant in the subtropical and subarctic regions,
where the reconstruction rates are high. 3) The optimum interpolation, taking account of eddy propagation, provides higher
reconstruction rates than that taking no account of the propagation. The effect of propagation on the optimum interpolation
is greater when it is applied to single-altimeter data than to multi-altimeter data.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
24.
T. Toyoda S. Masuda N. Sugiura T. Mochizuki H. Igarashi M. Kamachi Y. Ishikawa T. Awaji 《Deep Sea Research Part I: Oceanographic Research Papers》2009,56(4):495-512
Time-varying air–sea coupled processes in the central to eastern equatorial Pacific associated with strong El Niño development during the 1997–1998 period are examined using a newly developed reanalysis dataset obtained from four-dimensional variational ocean–atmosphere coupled data assimilation experiments. The time series of this data field exhibits realistic features of El Niño evolution. Our analysis indicates that resonance between eastward-propagating oceanic downwelling Kelvin waves and the seasonal rise of sea-surface temperature (SST) in the central to eastern equatorial Pacific generates relatively persistent high SST conditions accompanied by a deeper thermocline and more relaxed easterly winds than usual. The surface condition resulting from the wave-seasonal SST resonance represents a preconditioned state that leads to an enhancement in incident downwelling Kelvin waves to levels sufficient to induce large-amplitude unstable coupled waves in the central to eastern equatorial region. Heat balance estimates using our reanalysis dataset suggest that the unstable coupled waves are categorized within the intermediate regime of coupled Kelvin and Rossby waves and have the potential to grow rapidly. We argue that the seasonal resonance and the unstable coupled waves should play crucial roles in the development of the largest historical El Niño event, which was recorded between late 1997 and early 1998. 相似文献