Titlebook: New Developments in Mode-Water Research; Dynamic and Climatic Atsushi Kubokawa,Shang-Ping Xie,Humio Mitsudera Book 2013 Springer Japan KK,

Debrief

誘惑

Hideharu Sasaki,Shang-Ping Xie,Bunmei Taguchi,Masami Nonaka,Shigeki Hosoda,Yukio Masumotoelhafte Anwendung beider Ans?tze und Interpretation der Erge.Die schlie?ende Statistik ist die Wissenschaft davon, aus einer Stichprobe auf die Gesamtheit zu schlie?en. In ihr gibt es zwei vorherrschende Lehren: die klassische Statistik und die Bayes-Statistik. Die klassische Statistik verwendet zum

大約冬季

Masami Nonaka,Shang-Ping Xie,Hideharu Sasakielhafte Anwendung beider Ans?tze und Interpretation der Erge.Die schlie?ende Statistik ist die Wissenschaft davon, aus einer Stichprobe auf die Gesamtheit zu schlie?en. In ihr gibt es zwei vorherrschende Lehren: die klassische Statistik und die Bayes-Statistik. Die klassische Statistik verwendet zum

光明正大

Progress of North Pacific mode water research in the past decade,d; (3) impacts of the mode waters’ circulation and dissipation processes on the climate and biogeochemical processes; and (4) dynamic versus thermodynamic causes underlying the mode waters’ decadal changes. In addition to the review, future directions for mode water research are also presented.

財主

Review on North Pacific Subtropical Countercurrents and Subtropical Fronts: role of mode waters in ted to be important in addition to the variability of mode waters. STCCs exist in other oceans and they are also flanked by mode waters on their poleward sides, suggesting that they are maintained by similar dynamics.

A精確的

Mixed layer depth front and subduction of low potential vorticity water under seasonal forcings in nter, and the end of the period roughly corresponds to the disappearance of the MLD front in early spring. Subduction volume at the MLD front during this period is similar to that during 1 year in the steady-forcing model. Since the cooling of the deep mixed-layer water occurs only in winter and SST

Hot-Flash

DIS

Interannual variations of the Hawaiian Lee Countercurrent induced by potential vorticity variabilitrmal wind. The intensification and/or southward intrusion of the eastern subtropical mode water and subtropical mode water seem to have induced negative PV anomalies in 2003 and 2005, respectively. Using highresolution ocean simulations, we confirmed the migrations of PV anomalies and their contribu

VERT

,Interannual variability of the North Pacific Subtropical Countercurrent: role of local ocean–atmospk) cyclonic wind anomaly elevates (depresses) the thermocline and causes the fall (rise) in the SSH and SST, accelerating (decelerating) STCC to the south. It is suggested that the anomalies in the SST front and STCC in the preceding winter affect the subsequent development of the cyclonic wind anom

萬神殿

Response of the North Pacific subtropical countercurrent and its variability to global warming,ecays as CO2 concentrations double in the twenty-first century, owing both to weakened mode waters in the mean state and to reduced variability in mode waters. The reduced mode-water variability can be traced upstream to reduced variations in winter MLD front and subduction in the KOE region where m