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SUMATRA SQUALLS
SCOPE:• Overview
• Description
• Appearance
• Formation
• Locale
• Movement
• HAZARDS
SUMATRAS
OVERVIEW
“Sumatras” are lines of thunderstorms which usually occur
between March and November each year. (SW monsoon)
These squalls (lines of thunderstorms) develop at night
over Sumatra or the Malacca Straits and move east
towards Singapore and Peninsular Malaysia usually
during the pre-dawn and early morning.
They are often characterised by sudden onset of strong
gusty surface winds and heavy rain lasting from 1 to 2
hours as they move southwards along the west coast of
the Peninsular until it reaches Singapore in the early
morning.
Maximum gusts of up to 26 metres per second (93 km/h)
have been recorded during the passage of a Sumatra
squall.
CONDITIONS REQUIRED -TS
LIFTING AGENT/TRIGGER

HOW MANY HERE?

HOW ABOUT NIGHT?
SOUTH WEST MONSOON
Between April – September

(Inter monsoon – mid March/mid October)
Nights in the Straits of Malacca.
Conditions are ripe for thunderstorms. How?
MULTI CELLS
Although a thunderstorm can consist of just one ordinary cell that
transitions through its life cycle and dissipates without additional new
cell formation, thunderstorms often form in clusters with numerous cells
in various stages of development merging together. Unlike ordinary
single cells, cluster storms can last for several hours producing large
hail, damaging winds, flash flooding, and isolated tornadoes.
SQUALL LINES
Sometimes thunderstorms will form in a line which can extend
laterally for hundreds of miles. These "squall lines" can persist for
many hours and produce damaging winds and hail. The rain
cooled air or "gust front" spreading out from underneath the squall
line acts as a mini cold front, continually lifting warm moist air to
fuel the storms.
LOCAL PHENOMENAS
...NITE IN THE STRAITS
• DIURNAL VARIATION OF SURFACE
WIND
• KATABATIC WIND FROM SUMATRAN
& MALAYSIAN HIGHLANDS
• ADIABATIC COOLING
• CONVECTION & CONVERGENCE
• HI – RELATIVE HUMIDITY
Rapid formation of Squall lines
…SO WHEN NITE FALLS
HAZARDS
•
•
•
•

(Thunderstorms) HAIL
DAMAGING WIND
Wind shear at low levels.
Heavy precipitation that can last for a few hours.
Degrades aircraft performance (& nav systems)
• Lightning
Sumatras

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Sumatras

  • 1. SUMATRA SQUALLS SCOPE:• Overview • Description • Appearance • Formation • Locale • Movement • HAZARDS
  • 3. OVERVIEW “Sumatras” are lines of thunderstorms which usually occur between March and November each year. (SW monsoon) These squalls (lines of thunderstorms) develop at night over Sumatra or the Malacca Straits and move east towards Singapore and Peninsular Malaysia usually during the pre-dawn and early morning. They are often characterised by sudden onset of strong gusty surface winds and heavy rain lasting from 1 to 2 hours as they move southwards along the west coast of the Peninsular until it reaches Singapore in the early morning. Maximum gusts of up to 26 metres per second (93 km/h) have been recorded during the passage of a Sumatra squall.
  • 5. LIFTING AGENT/TRIGGER HOW MANY HERE? HOW ABOUT NIGHT?
  • 6. SOUTH WEST MONSOON Between April – September (Inter monsoon – mid March/mid October) Nights in the Straits of Malacca. Conditions are ripe for thunderstorms. How?
  • 7. MULTI CELLS Although a thunderstorm can consist of just one ordinary cell that transitions through its life cycle and dissipates without additional new cell formation, thunderstorms often form in clusters with numerous cells in various stages of development merging together. Unlike ordinary single cells, cluster storms can last for several hours producing large hail, damaging winds, flash flooding, and isolated tornadoes.
  • 8. SQUALL LINES Sometimes thunderstorms will form in a line which can extend laterally for hundreds of miles. These "squall lines" can persist for many hours and produce damaging winds and hail. The rain cooled air or "gust front" spreading out from underneath the squall line acts as a mini cold front, continually lifting warm moist air to fuel the storms.
  • 10. ...NITE IN THE STRAITS • DIURNAL VARIATION OF SURFACE WIND • KATABATIC WIND FROM SUMATRAN & MALAYSIAN HIGHLANDS • ADIABATIC COOLING • CONVECTION & CONVERGENCE • HI – RELATIVE HUMIDITY
  • 11. Rapid formation of Squall lines
  • 13. HAZARDS • • • • (Thunderstorms) HAIL DAMAGING WIND Wind shear at low levels. Heavy precipitation that can last for a few hours. Degrades aircraft performance (& nav systems) • Lightning