Search results
Results From The WOW.Com Content Network
The Java Sea covers the southern section of the 1,790,000 km 2 (690,000 sq mi) Sunda Shelf. A shallow sea, it has a mean depth of 46 m (151 ft). A shallow sea, it has a mean depth of 46 m (151 ft). It measures about 1,600 km (990 mi) east-west by 380 km (240 mi) north-south [ 4 ] and occupies a total surface area of 320,000 km 2 (120,000 sq mi).
[7] [6] When the sea level was decreased by 30–40 meters or more, land bridges connected the islands of Borneo, Java, and Sumatra to the Malay Peninsula and mainland Asia. [2] Because the sea level was 30 meters or more lower throughout much of the last 800,000 years, the current status of Borneo, Java, and Sumatra as islands has been a ...
The river rises from its source in central Java at the Lawu volcano, then flows north and eastward to its mouth in the Java Sea near the city of Surabaya. Other major rivers are Brantas, Citarum, Cimanuk and Serayu. [citation needed] The average temperature ranges from 22 °C (72 °F) to 29 °C (84 °F); average humidity is 75%.
East Java province borders the Java Sea in the north, ... The average temperature ranges between 19–34 °C. Temperatures in the lower mountain areas, and even in ...
Although air temperature changes little from season to season or from one region to the next, cooler temperatures prevail at higher elevations. In general, temperatures drop approximately 1 °C per 90-meter increase in elevation from sea level with some high-altitude interior mountain regions experiencing night frosts.
The rise of sea level during a meltwater pulse 14,600 to 14,300 years Before Present was as much as 16 meters within 300 years. [6] Present sea levels submerge a number of Pleistocene paleo river systems that drained much of Sundaland during the last glacial maximum 18,000 to 20,000 years ago. [7] To the east of the Sunda Shelf is the Sahul Shelf.
Graph showing ocean temperature versus depth on the vertical axis. The graph shows several thermoclines (or thermal layers) based on seasons and latitude. The temperature at zero depth is the sea surface temperature. The ocean temperature plays a crucial role in the global climate system, ocean currents and for marine habitats.
The ocean surface of this part of the far western Pacific is on average each day higher than that in the adjacent part of the Indian Ocean. The difference drives upper thermocline water "downhill" through the deep, straight, westerly, north–south Makassar Strait then to meet the in reality combined Java Sea-Banda Sea.