South China Sea Warm CurrentZhe-Min Coastal CurrentKuroshioSouthwestern Taiwan StraitOxygen isotope (δ18O) of seawater is an excellent proxy for tracing the origins of water masses and their mixing processes. Combining with hydrographic observation, hybrid coordinate ocean model (HYCOM) analysis data...
Hainan Island was known as the South China Sea on a "Pearl". In a sea of bright sunshine and warm in winter in Hainan, no real hot summer and cold winter. Is a winter swimming and a refuge from resort. Four seasons Evergreen on the island, air purifiers, known as "the good place...
Warmer ocean waters can contribute to more powerful tropical storms and impact marine life. In addition, a warmer atmosphere holds more moisture and can increase potential flooding events. Melting sea ice in the Arctic is also cau...
Each wooden house is a 2-storey duplex structure with a spacious living room on the first floor and a warm room on the second floor. The large floor-to-ceiling Windows ensure plenty of light and provide excellent viewing angles. In your spare time, you can drink and chat in the living ...
In addition, dipolar SST anomalies in the Indo-Pacific warm pool can help to sustain the WPSH intensification through a positive feedback3. Consequently, the SLP EOF-1 can be viewed as an air–sea interaction mode in the tropical oceans. On the other hand, EOF-2 strongly represents a ...
Persistent warm-eddy transport to Antarctic ice shelves driven by enhanced summer westerlies Article Open access 22 January 2024 Introduction The South China Sea (SCS) is the largest semi-enclosed marginal deep sea located west of the North Pacific (NP) (Fig. 1), and its circulation patterns ...
Cold filaments (CFs) in the southwestern South China Sea (SCS) impact local hydrodynamics and the ecological environment. In this study, the effects of typhoons passing over the northern SCS on CFs are investigated using multi-source observational and re
This warm water affects the weather. It is always raining over El Nino. El Nino contains a lot of energy. Scientists think this energy is formed when wind comes from the northern half of the world. The winds blow across warm sea water in the south. When the strong wind hits the warm ...
Just as today’s world is not uniformly 1.2°C warmer than the pre-industrial, a 3°C world is not uniformly 1.8°C warmer than today (see chart 3). Some regions, chiefly the oceans and parts of South America, will warm less; others will get much hotter. The Arctic, including norther...
The North Pacific subtropical gyre (NPSG) plays a major role in present global ocean circulation. At times, the gyre has coursed through the South China Sea, but its role in the evolutionary development of that Sea remains uncertain. This work systematically describes a major shift in NPSG pal...