In this study, we performed numerical experiments with an eddy-resolving ocean general circulation model and investigated oceanic responses to cold- and warm-season atmospheric forcing, focusing on the Kuroshio and North Pacific subtropical mode water (STMW) in the western mid-latitude North Pacific....
13. The CYF is strongest in the winter when it consists of a northern warm-tongue in the east where high-temperature and high-salinity water of TWW origin expands northwestward and a southern cold-tongue in
The larger errors of temperature and salinity in the western Pacific may partly be due to the mismatch of model and real topography. Simulated currents and Atlantic meridional overturning circulation (approximately 25 Sv at 40°N) are comparable to other OGCM simulations. Figure 1 Open in figure ...
For example, when a hybrid-type construction machine is driven in cold climates, a warm-up operation is carried out until the engine is warmed up because the engine is cold at a time of starting the engine. The hybrid-type construction machine may acquire power for operations (i.e., ...
a number of processes can occur to modify the hydrographic structure through the generation of vertical motion. For example, ice-front melting and subglacial discharge often create rising cold fresh buoyant plumes, while fluvial discharge from side-entry glaciers or supraglacial meltwater contribute to...
and Variability Impact on Regional Hydrological Regimes and Water AvailabilityDrinking Water Quality: Accelerating the Process of Water Pollution ManagementFeature PapersHydroacoustics in Marine, Transitional and FreshwatersHydrological Modelling and Remote Sensing: Selected Papers from the 2017 and 2018 SWAT ...
Moreover, in warm pool and SPCZ where the frequency of WPC is over 12%, the SST is over 302 K (Figure 2a). The WPC frequency in general follows the underlying SST distribution. The lower SST in the South-east Pacific is influenced by the sea currents and generates less precipitation. ...