- JIPS Sittwe Camp Profiling Report
- Statement of INGO’s in Myanmar, 31 August 2017 [EN/MY]
- Advisory Commission on Rakhine State: Final Report, August 2017
- RW Topics: Refugees/Migrants - South-East Asia
Appeals & Funding
- 2017 Humanitarian Needs Overview
- 2017 Humanitarian Response Plan
- Humanitarian Action for Children 2017: Myanmar
- Country-based Pooled Fund
- UNHCR Global Focus
- OCHA Myanmar
- UNHCR Operational Portal: Thailand-Myanmar Cross Border Portal
- UNFPA: Myanmar 2014 Population and Housing Census
- Internal Displacement Monitoring Centre (IDMC)
- Advisory Commission on Rakhine State
- Department of Meteorology and Hydrology
- Food Security Cluster: Myanmar
- Human Rights Watch: Myanmar - Events of 2016
- Myanmar: Floods and Landslides - Jul 2017
- Tropical Cyclone Mora - May 2017
- Myanmar: Floods - Jun 2016
- Tropical Cyclone Roanu - May 2016
- South-East Asia: Drought - 2015-2017
- Tropical Cyclone Komen - Jul 2015
- Myanmar: Floods and Landslides - Jul 2015
- Myanmar: Floods - Jul 2014
- Myanmar: Floods - Aug 2013
- Tropical Cyclone Mahasen - May 2013
This website allows you to explore how different scenarios of global greenhouse gas emissions and adaptation to climate change could change the geography of food insecurity in developing and least-developed countries. By altering the levels of future global greenhouse gas emissions and/or the levels of adaptation, you can see how vulnerability to food insecurity changes over time, and compare and contrast these different future scenarios with each other and the present day.
Recurrent earthquakes, floods, typhoons, and volcanoes present significant challenges to vulnerable populations in the East Asia and the Pacific (EAP) region. Some countries also face civil unrest and associated humanitarian impacts, as well as limited government capacity to respond to disasters. Between FY 2007 and FY 2016, USAID’s Office of U.S. Foreign Disaster Assistance (USAID/ OFDA) and USAID’s Office of Food for Peace (USAID/ FFP) provided humanitarian assistance in response to a diverse range of natural and complex emergencies in the region.
The gFSC global dashboard provides a quick snapshot of the country-level Food Security Clusters around the world. The updated dasboard shows that as of October 2015, the country-level Food Security Clusters remain only at 52 percent funded against their yearly requirements
New Zealand’s aid programme aims to make a positive difference in people’s lives‚ demonstrated through tangible‚ measurable results. To do this‚ we need a plan that outlines our ambition and focus.
Using an innovative approach with GIS and remote sensing, the Oak Ridge National Laboratory LandScanTM is the community standard for global population distribution. At approximately 1 km resolution LandScan is the finest resolution global population distribution data available and represents an ambient population (average over 24 hours).
Temperatures in the Asia-Pacific region can go very high with central India reaching 50oC or more. The Tibetan plateau rarely exceeds 20oC because of its high elevation.
These temperatures are based on average highs over a period of approximately 50 years. Maximum temperatures in the region may therefore be from different months of the year and a temperature in any given location may exceed these maximums.
Köppen-Geiger Climate Classification
The highly referenced climate classification map of Wladimir Köppen was published for the first time in 1900 and updated in its latest version by Rudolf Geiger in 1961.
Climate classification is applied to a broad range of topics in climate and climate change research as well as in physical geography, hydrology, agriculture, biology and educational aspects.
The Human Footprint
Human influence on the earth’s land surface is a global driver of ecological processes on the planet, en par with climatic trends, geological forces and astronomical variations. The Wildlife Conservation Society (WCS) and the Center for International Earth Science Information Network (CIESIN) at Columbia University joined together to systematically map and measure the human influence on the earth’s land surface today.
This map shows the average amount of precipitation falling in a year, based on approximately 50 years of data. The figures shown do not therefore represent the amount of precipitation that may occur in any given year.
Elevation and Bathymetry
The region is home to the world's highest mountain, Mount Everest (Sagarmatha in Nepal and Chomolungma in China) at 8,848m, as well as the deepest surveyed point in the oceans,
Challenger Deep in the Marianas Trench at 10,911m.
Tectonic Plates and Fault Lines
The region is home to extremes in elevation and the world's most active seismic and volcanic activity. Southwest of India, the Maldives has a maximum height of just 230cm, while far to the north, the Tibetan Plateau averages over 4,500m across its 2.5 million square kilometres and is home to all 14 of the world's peaks above 8,000 metres. The Himalaya were born 70 million years ago when the Arabian Plate collided with the Eurasian plate.
Volcanic Explosivity in Asia-Pacific
This map shows the density of volcanic eruptions based on the explosivity index for each eruption and the time period of the eruption. Eruption information is spread to 100km beyond point source to indicate areas that could be affected by volcanic emissions or ground shaking.
Earthquake Intensity Risk Zones
This map shows earthquake intensity zones in accordance with the 1956 version of the Modified Mercalli Scale (MM), describing the effects of an earthquake on the surface of the earth and integrating numerous parameters such as ground acceleration, duration of an earthquake, and subsoil effects. It also includes historical earthquake reports.