Atmospheric, hydrological, or oceanographic in nature and may cause loss of life
Flood
Overflow of water onto normally dry land in an existing waterway, such as a river, stream, or drainage ditch
Stormsurge
Abnormal sea level rise occurring during tropical cyclones or "bagyo," caused by the strong winds and low atmospheric pressures that tropical cyclones produce
Mature stage of a cumulus cloud
Cloud becomes very large, the water in it becomes large and heavy, and raindrops start to fall through the cloud when the rising air can no longer hold them up
Dissipating stage of a cloud
Downdrafts in the cloud begin to dominate over the updraft, and cloud droplets can no longer form
Thunderstorm
Violent, short-lived weather disturbance that is almost always associated with lightning, thunder, dense clouds, heavy rain or hail, and strong, gusty winds
Factors that contribute to flooding
Rainfall intensity and duration, as well as slow-moving thunderstorms
ElNiño
Significant increase in ocean temperature over the eastern and central Pacific Ocean
Typhoon
Intense circular storm that originates over warm tropical oceans and is characterized by low atmospheric pressure, high winds, and heavy rain
Hazardmap
Highlights areas that are affected by or are vulnerable to a hazard, such as earthquakes, volcanoes, landslides, flooding, and tsunamis
Type of rain gauge wherein a funnel collects the rain and sends electrical signals to the receiver when it reaches a certain amount of precipitation
PAGASA publishes regularly updated color-coded satellite images generated from Himawari-8, a geo-stationary weather sattelite that that visualizes rain distribution in the Philippines
DOST-NOAH is a program of the Department of Science and Technology (DOST) that advances the use of cutting-edge technology in disaster prevention and mitigation efforts
Areas with low pressure generally have a bad weather
Thermometer
Used to measure how hot or cold the surrounding air is
Wind vane
Used to measure wind direction
Barometer
Measures atmospheric pressure
A meteorologist would use a wind vane or a wind finding radar to measure wind direction and a thermometer to measure temperature
Republic Act (RA) 10121 provides a comprehensive, all-hazard, multi-sectoral, inter-agency, and community-based approach to disaster risk management
Disaster Risk Reduction and Management (DRRM)
Main objective is to build a resilient community that can effectively respond to and recover from disasters
Response
Post-event disaster risk element that involves the provision of emergency services and public assistance during or immediately after a disaster
Correct sequence of pre-event elements of disaster risk reduction
1. Prevention
2. Mitigation
3. Adaptation
4. Preparedness
The ultimate effect of proper Disaster Risk Reduction (DRR) approaches and tools is conducting effective disaster response while reducing the risks of similar disasters occurring again
The major concerns of disaster risk reduction management involve citizens or everyone within the community
Clear and simple risk communication increases confidence in acting to make individuals safer
Proposing laws and policies to disaster is not a priority concern of disaster risk reduction action
Proper planning and harmonizingmessages are key elements to avoid confusion in an organization for disaster risk reduction awareness
Sinkhole
Depression in the ground that results from the collapse of the surface layer of the soil
Gravity plays a crucial role in landslides
Steeper slopes can lead to faster landslides, but the distance to the debris may not necessarily be nearer
Volcaniceruptions
Can trigger landslides by altering minerals to clay, releasing volcanic gases that weaken rocks, and causing vibrations that loosen surrounding soil
Areas that have previously experienced landslides are more prone to future landslides
While certain signs may indicate an impending geologic hazard, they are not definitive proof of an imminent event
Soilliquefaction
Ground failure or loss of strength that causes otherwise solid soil to behave temporarily as a viscous liquid, is a natural cause of landslides as it destabilizes slopes
Soil nutrients generally affect the stability of a slope in the context of landslides
Tsunamis are not direct effects of landslides. They are usually caused by underwater earthquakes or volcanic eruptions
Blastingtechniques used in mining can produce vibrations that weaken soil, contributing to landslides
Dissolutionsinkholes
Typically caused by the gradual dissolution of carbonate rock (e.g., limestone) by acidic water
Water is a natural agent of erosion
Flows and loosens the soil, contributing to landslides
Soil creep
Type of landslide characterized by very slow movement that is hardly noticeable