Using mooring observations inside the Makassar Strait, Susanto et al. First, we strive to quantify the interannual modulations of the intraseasonal eddy variability inside the CS by introducing an appropriate index. In addition to the 40‐ to 60‐day oscillations, the low‐frequency salinity variability in the Makassar Strait is also subject to the ENSO‐modulated circulation changes. Exploring the Inner Space of the Celebes Sea 2007 . Figure 15a compares S′(t) and the best‐fit What cities are in Prowers County Colorado, Where is Pitkin County Colorado? Where is Sulu Sea? From Figure 5, it is clear that the intensity of the 40‐ to 60‐day oscillation inside the CS changes from year to year. What cities are in Chaffee County Colorado, Where is Baca County Colorado? As a result, all of the water entering the Celebes Sea stays shallow and flows out of the Celebes Sea through the Makassar Strait, between the islands of Borneo and Sulawesi. Number of times cited according to CrossRef: Annual versus semi-annual eddy kinetic energy variability in the Celebes Sea. Borneo 4. and you may need to create a new Wiley Online Library account. This map shows the location of the Philippines within Asia, specifically Southeast Asia. Celebes 8. Where is Celebes Sea? Like their spatial patterns, the two PC time series, shown by the dark black lines in Figures 2b and 2d, also match very favorably with a linear correlation coefficient reaching r = 0.96. The Molucca Sea has a total surface area of 77,000 square miles (200,000 square km). What cities are in Hartford County, Where is Fairfield County Connecticut? What cities are in Las Animas County Colorado, Where is Larimer County Colorado? Journal of Geodynamics. (c, d) Same as (a, b) except from the Estimating the Circulation and Climate of the Ocean, Phase II simulation. A sea lily (crinoid) pointed in the direction of the current. As such, before exploring the dynamical processes governing the interannual modulations of eddy variability inside the CS, it is important to verify the broadscale oceanic variability surrounding the CS in the ECCO2 state estimate against the available satellite altimetry measurements. To emphasize this point, we plot by the red lines in Figure 7 the EKE time series inside the CS basin (117°E–125°E, 1°N–6°N) based on the surface velocity data that is high‐pass filtered at 100 days. There are three objectives in our study. The Celebes Sea (CS), also known as the Sulawesi Sea, is a choke point where the western Pacific Ocean circulation and water masses are connected and intermingled to those in the eastern Indian Ocean. Since it is constructed in a dynamically and thermodynamically consistent way (see section 2) and produced adequately the intraseasonal eddy variability inside the CS, the ECCO2 state estimate is well suited to explore the interannual modulations of the CS 50‐day oscillations. (The TOPEX/Poseidon and its subsequent Jason satellite missions have repeat cycle of 9.9156 days. The Celebes Sea is a piece of an ancient ocean basin that formed 42 million years ago in a locale removed from any landmass. Gezilecek Yerler What cities are in Eagle County Colorado, Where is Dolores County Colorado? Physics, Comets and The Sulawesi Sea covers an area of 400,000 km2, with mean water depth of somewhat over 5 km and crustal thickness of about 6-7 km (Murauchi et al., 1973). Customized Celebes Sea maps. Required fields are marked *, Nerede Çekiliyor This repeat cycle aliases the semidiurnal M2 tides, for example, into the 62.1‐day altimeter‐derived sea surface height [SSH] signals [Ray, 1998].) 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