Sea level rise and fall can occur once a day (single tide or diurnal tide). Or twice a day (double or semi-diurnal tide). While the tide between the two is known as mixed tide. The tidal range is the difference between the water level at maximum tide. And the water level at the time of minimum tide which is also influenced by the geometry of the area in question. It will show season in West Papua.
Physical Aspects of Waters And Seasons in West Papua
Tides in Papua waters reach 3 – 6 meters, with mixed double tides. Ocean waves are formed due to the transfer of energy from the wind to the surface sea, or at certain times caused by an earthquake on the seabed. This wave propagates in all directions carrying energy which is then released to the beach in the form of waves.
Observations of waves in Papua waters have not been widely carried out. However Thus, there is actually a relationship between monsoons and wave motion patterns. Waves that come towards the beach can cause a nearshore current) which affects the process of sedimentation or abrasion on the beach, also effect for season in West Papua.
This beach is mainly determined by the magnitude of the angle formed between the waves that come up with a coastline. If the angle of incidence is large enough, a current will be formed long the coast (longshore current) caused by differences in hydrostatic pressure.
Apart from waves, tides are another important oceanographic parameter as a current generator on the coast.
The current caused by the tide is affected by bottom of the water. The strongest tidal currents will be found near the surface and will its speed decreases the closer it gets to the bottom of the water and can effect season in West Papua.
Current is the movement of water that results in horizontal. And also vertical displacement mass of water by the difference in potential energy. The state of ocean currents generally occurs due to the influence of several simultaneous forces consisting of fixed currents, periodic currents, (tidal) and currents wind.
Seasons in West Papua
Waters in Papua are strongly influenced by two season in West Papua., namely: (a) the west season, and (b) east season. The west season peaks in February, while the east season peak occurs in August. Physical, chemical, and biological properties of waters in both. Read also the Forest and Land Resources Forest Area Of West Papua that you need to know.
During the season, in the west, the sea surface temperature tends to be hotter than in the east monsoon. The cold surface temperature in the east monsoon tends to make the waters tend to more fertile. Namely with an increase in phytoplankton and zooplankton.
The southern waters of Papua are waters that have the characteristics of: water mass that is somewhat different from the waters of other Indonesian territories. This is due to by the geographical location of these waters which are adjacent. And more open to the Banda Sea, Timor Sea and Indian Ocean. This the detail about two season in West Papua.
In the east monsoon, the oceanographic conditions of these waters are plentiful influenced by water masses from the Banda Sea (Wyrtki, 1961; Tchernia, 1980). This matter has a major effect on the distribution of chlorophyll-a. And nutrients as well as pelagic fish in. So that these waters are also known as one of the fishing areas and shrimp, especially fish.
There are explanation about season in West Papua. This two seasons that papua have is so unique and nice. This information will give you more knowledge. Now you know about west papua. Hope this article is useful for who needed this information.
