INDONESIAN WETLANDS
DIAN DWI KARTIKASARI
BERBAK NATIONAL PARK
Located around 51 km from the provincial capital of Jambi, Central Eastern Sumatra, Indonesia.
lat lon title -1.383333
104.3333 Berbak National
Park
BERBAK NATIONAL PARK
Source: Boku Surtanal, mapping and survey agency
BERBAK NATIONAL PARKSources of Water
Soil Type, Peat Distribution and Carbon Stock of Berbak Natinal Park
Source : Wetland International and World Resource Institute
BERBAK NATIONAL PARK
(by : Jambi University)
BERBAK NATIONAL PARK
Tanjung Puting National Park
Source of Water : Kumai River and Seruyan River
The park is a world icon for orangutan (Pongo pygmaeus) rehabilitation and conservation efforts.
It is home to 220 species of birds, 17 species of reptiles and 29 species of mammals, a total of tress are 2390
Tanjung Puting National Park
C-stocks in riverine peat swamp forests of Tanjung Puting National Park, by distance from the river
Source : Center for International Forestry Research (2009)
Tanjung Puting National Park
Services
Tanjung Puting National Park
Karimun Jawa Archipelago
Location: 70 km off the north coast of Central Java, Lat :-5.78333333 Lon :110.35 (en.wikipedia.org)
Area: 7,026 ha.
Principal vegetation: Mangrove forest
Karimun Jawa Archipelago
Source of water : Java Sea
The islands have been designated as a Marine Nature Reserve
Average temperatures range : 20-30°C
Source : indahnesia.com
Land use : Wildlife conservation; there is some agriculture on the inhabited islands and fishing in the surrounding waters. Possible changes in Land use: There is a project to develop rice cultivation and aquaculture (fishponds) on the islands.
Karimun Jawa ArchipelagoCarbon Storage : 1,0667x 1015 g C/yr (Duarte & Chiscano, 1999)
Services
Karimun Jawa Archipelago
Regulating services. These include regulation of climate, natural hazards such as floods, disease, wastes, and water quality
Cultural services. These include recreational, esthetic. Coastal tourism is the fastest-growing sector of the global tourism industry, and is a major part of the economies
Supporting services. These include soil formation, photosynthesis, and nutrient cycling by healthy ecosystems, which support goods and services used more directly by humans
Water BalanceP = ET + RO + I ± ΔS
P = Precipitation (mm/day)ET = Evapotranspiration (mm/day)RO = Run-off (mm/day)I = Infiltration (mm/day)ΔS = Water Balance (mm/day)www.gtz.deindonesia
Variable Berbak National Park Tanjung Puting National Park P (mm/day) 6,75 6,75ET (mm/day) 3,56 11,08RO (mm/day) 5,19 3I (mm/day) 0,2 - ΔS (mm/day) -2,2 -References E. Siderus and J, Van Denberg Takahashi et al (2000)
Climate Change in Indonesia
Hulme dan Sheard, 19990
Rainfall in 2080
The annual rainy season may be delayed for 30 days.and there may be a 10% increase in rainfall in the crop year (April-June), and Will increase of more than 75% in summer (july to september)
Temperature in 2020
Susandi (2007)
Temperature will increase starting from 0,36 to 0,47 in 2020. The higghest temperatureoccurs in Borneo Islands and Maluku
Indonesia's exposure to seismic, volcanic and tropical storm hazard (OCHA 2007)
Climate Change in Indonesia
The Disappearing of Coastal Land
JakartaCoastalRegionin 2050
Climate Change in Indonesia
BERBAK NATIONAL PARK
Climate Change in Indonesia
Climate Change : Action
Tanjung Puting National Park
Denuded mangroves could be restored by involving communities whose livelihoods depend on them
Karimun Java Archipelago
Climate Change in Indonesia
Changes in wind patterns could affect coastal and estuarine circulation patterns and upwelling or downwelling of water in marine systems
Changes in the frequency and intensity of storms would affect watercirculation processes and threaten coastal aquaculture and fishing industry facilities
Changes in precipitation could flood coastal systems or leave them indrought
WWF is pushing for agreements and policies that protect sensitive marine habitats and species from inevitable effects of climate change.
Research to assess the potential and increase the absorption of CO2 from the marinesector by plankton, coral reefs and sea grass
REFERENCES
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