America S. East Oceania. East Oceania All the countries. Climate - Indonesia Average weather, temperature, rainfall, when to go, what to pack. Some consider Western New Guinea as part of Oceania, and in this case, Indonesia would be a transcontinental country. The climate of Indonesia is almost everywhere equatorial , ie hot, humid and rainy throughout the year. In some areas, there is a dry season, more or less marked, which is therefore the best period for a trip.
As usually happens in hot countries, the rains occur in the form of downpours or thunderstorms, which sometimes can cause flooding. There are also mountains and volcanoes, often very high, where the temperature naturally decreases with altitude. Unfortunately, the country is also vulnerable to threats posed by global warming and climate change.
The climate of a location or region is affected by its latitude, altitude, terrain, and nearby water bodies and their currents. There is variation in climate across different parts of the world. These variations are mostly due to natural processes or external factors such as persistent changes to the atmosphere or changes in land use. There are extreme variations in rainfall, especially when comparing the dry season June to September to the rainy season November to March. It should be noted, however, that climate is not temperature.
Climate is an entity on its own while temperature is a variable of climate; other variables include humidity, precipitation, cloudiness, visibility and, wind.
There are three different climates that can be found in Indonesia. The primary climate in Indonesia is tropical rainforest, which has the highest level of precipitation, followed by tropical monsoon and tropical savanna which have lower levels of precipitation.
The western and northern parts of Indonesia have the most precipitation. Elevation has a major impact on the climate. As elevation increases, pressure decreases. As pressure decreases, air molecules spread out further leading to a decline in temperature. The lowest point in Indonesia is in southern portion of the Philippine Trench, east of Miangas. It is 9, meters below sea level. The highest point in Indonesia is Puncak Jaya at 4, meters above sea level.
Indonesia has a mean elevation of meters above sea level. The wet and dry seasons are the two major seasons experienced in Indonesia, and the climate differs across its various islands. The west coast of Sumatra gets above centimeters of rain per year. Other islands that receive much rain include Kalimantan, Java, Papua, and some parts of Sulawesi, while islands such as Sumba and Timor receive less rain.
The climate of Indonesia and its neighboring countries are mostly alike because there are similarities in the times of year that seasons occur. Furthermore, most of these countries experience tropical climates as well.
It is comprised of approximately 17, islands. Indonesia is considered to be at serious risk from projected effects of climate change. This is a figure which is predicted to further rise by the end of the century, thereby affecting businesses. This will raise the frequency of droughts and food shortages and change the precipitation patterns of the wet and dry seasons. Indonesia is south of the typhoon belt which includes the Philippines, Vietnam, China, and Japan.
Since Indonesia is close to the equator and surrounded by much water, its climate is a tropical marine climate with light winds and frequent thunderstorms. Temperature and rainfall vary across its different islands due to elevation and monsoon patterns. The dry season is mainly influenced by the Australian continental air masses while the wet season is influenced by air masses from mainland Asia and the Pacific Ocean.
Taking into consideration Indonesian climate, it is best for tourists to visit between May and September. The city of Bogor, near Jakarta, lays claim to having to world's highest number of rainstorms per year On the other hand, the islands closest to Australia--including Nusa Tenggara and the eastern tip of Java--tend to be dry, with some areas experiencing less than 1, millimeters per year.
To complicate the situation, some of the islands of the southern Malukus experience highly unpredictable rainfall patterns, depending on local wind currents. Although air temperature changes little from season to season or from one region to the next, cooler temperatures prevail at higher elevations. The highest mountain ranges in Irian Jaya are permanently capped with snow. Located on the equator, the archipelago experiences relatively little change in the length of daylight hours from one season to the next; the difference between the longest day and the shortest day of the year is only forty-eight minutes.
The boundary between the western and central time zones--established in is a line running north between Java and Bali through the center of Kalimantan. The border between central and eastern time zones runs north from the eastern tip of Timor to the eastern tip of Sulawesi.
Indonesia Table of Contents The main variable of Indonesia's climate is not temperature or air pressure, but rainfall.
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