organized, rotating system of clouds and thunderstorms that initially form over tropical ocean waters
TYPHOONS
formed over the northwest Pacific.
HURRICANE
In the Atlantic and the east Pacific
TROPICAL CYCLONE
In the Indian Ocean and south Pacific
EYE
calmest portion of any storm and point at which winds rotate. Winds converging toward center are deflected by Coriolis force
MAXIMUM SUSTAINED WINDS
Located closest to eye of storm, in an area called eyewall or wall cloud
TROPICAL DERESSION
weakest form of tropical cyclone
TROPICAL STORM
when depression intensifies and attains sustained winds of 62 km/h
TYPHOON
when tropical cyclone sustained winds reach 118 km/h
PUBLIC STORM WARNING SIGNAL (PSWS)
issued in affected areas to inform public on projected impacts of storm and how soon these are expected to be felt.
THUNDERSTORM
weather condition characterized by heavy rain and wind accompanied by lightning, thunder; sometimes with hail and tornadoes.
It can last for 30 minutes to several hours.
Require moisture and rapidly rising warm air, which is why they are common in humid areas.
They are frequently observed near equator and rarely in polar regions.
CONVECTION
key mechanism in thunderstorm formation. Warm air near ground rises and cooler air sinks. Warm surface air will continue to rise since less dense than surrounding air.
UPDRAFT
Rising Air
DOWNDRAFT
Downward moving air
LIGHTNING
Plasma travels downward to create a path for current to flow electrons surge down to meet streamers
THUNDER
shockwave caused by this explosion, which manifests as a loud booming sound
SEVERE
if it contains wind gusts of at least 94 km/h, hail at least an inch in diameter, or a tornado
SINGLECELL THUNDERSTORM
short-lived storm consisting of a single updraft-downdraft 18couplet. It is capable of producing heavy rainfall and lightning
MULTI-CELL THUNDERSTORM
system of individual cells. Each cell usually lasts for 30 minutes to an hour, while the entire system can last for hours.
SUPERCELL THUNDERSTORM
highly organized thunderstorm with a large rotating updraft that can be 20 km in diameter and 15 km in height. It can last for several hours and produces violent tornadoes.
SQUALL LINE
group of storms arranged in a straight line. It is shorter-lived than multi-cells and supercells, and are less likely to produce tornadoes
THUNDERSTORM WATCH
when thunderstorm formation is likely within next twelve hours
THUNDERSTORM ADVISORY
When there is indication that a thunderstorm is threatening a specific area within next two hours
WATERSPROUT
or a tornado that originated from a water body.
STREAMERS
objects on ground reach out to the clouds by growing finger-like electrical discharges.
FLOODING
when areas usually not covered by water are engulfed or submerged.
usually caused by a temporary rise in or overflowing of streams, rivers, or confined bodies of water.
Failure of manmade structures such as dams and clogging of drainage systems are common causes.
typically develop in a span of hours to a few days
FLASH FLOOD
In cases wherein there is rapid inundation (less than six hours)
FACTORS THAT INFLUENCE FLOODING
rainfall intensity and duration, topography, soil conditions, and ground cover.
SURFACE RUNOFF
water that does not enter soil and moves downslope, is more dominant in impermeable materials such as clay, or in cases where soil is too saturated to allow infiltration.
FLOOD HAZARD MAPS
used to anticipate degree of flooding in an area and extent of damage that the event can cause
AERIAL PHOTOGRAPHS AND SATELLITE IMAGES
to produce a preliminary flood hazard map.
involves analysis of geology and morphological characteristics (geomorphology) of area.
GEOGRAPHIC INFORMATIONSYSTEM (GIS) SOFTWARE.
allows integration and analysis of geographic or spatial data and organizes them to visualizations sucha as maps.
Google Earth is an example
Nationwide Operational Assessment of Hazards (NOAH)
program for disaster research development makes use of advanced technologies, provides information services for improved disaster risk reduction and mitigation.
makes use of GIS software, simulations and models, and crowd sourcing of flood events to create flood hazard maps
STORM SURGES
abnormal rise in seawater level during a storm.
the water undergoes wave shoaling.
natural flow of water from sea to shore is delayed by friction between water & seabed, causing to pile up.
driven by the force of storm winds
RED (TAKEACTION)
Storm surge is CATASTROPHIC. there is significant threat to life. Mandatory evacution is enforced
ORANGE (ALARM)
EXPECTED. Conditions become life threatening.
All marine activities must be cancelled
YELLOW (ALERT)
POSSIBLE. Stay away from coast or beach.
Preparation measures must be carried out
GREEN (NO ALERT)
no action required
EL NINO AND LA NINA
warm and cold phases of the El Niño-Southern Oscillation (ENSO) cycle.
ENSO CYCLE
changes in oceanic and atmospheric temperatures in Equatorial Pacific.
significantly affects not only ocean processes, but also rainfall, wind, and tropical cyclone patterns
SOUTHWEST/SUMMER MONSOON
locally known as Habagat, is a warm, moist air originating from the southwest Indian Ocean.
associated with heavy rainfall and humid climate
NORTHEAST/WINTER MONSOON
known as Amihan come from Mongolia and northwestern China. Amihan is characterized by moderate temperatures, and little to no rainfall
EL NIÑO
Spanish term translates to “TheLittleBoy” or “ChristChild.” originally observed in Southern America as unusually warm seawater
named such because phenomenon typically occurs around Christmas.
usually starts between December and February.
indicated by a delayed onset or early termination of the rainy season, and weak monsoon and tropical cyclone activity.
in Philippines, brings fewer and less intense storms, but also associated with severe dry spells or droughts which can be just as damaging.
WATER SUPPLY
A primary concern during El Niño season
LA NIÑA
means “TheLittleGirl,” characterized by sea surface temperatures lower than average.
also referred to as El Viejo (The Old Man) or anti-El Niño, since local effects on weather are generally opposite of those of El Niño.
caused by upward movement of cold water by unusually strong trade winds and ocean currents in a process called upwelling.
in Philippines is correlated with destructive typhoons, heavy rainfall, and associated landslides and floods