Bengal Convective Outlooks
March-May 2006
Jonathan
D. Finch
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Forecasts will normally
be updated between 3 UTC and 6 UTC(0900-1200 BST) since surface based convective
initiation
is generally between 9
and 11 UTC. These are updated as needed through initiation time.
In particularly active periods
I may update several times
per day. If violent tornadoes are expected, I will try to issue tornado
watch boxes before events
unfold--time permitting.
2006 Convective Outlooks
Apr 18 2006
Day 1 no
risk of high-end severe storms
Apr 19 2006
Day 2 slight
risk of high-end severe storms
Apr 20 2006
Day 3 slight
risk of high-end severe storms
Apr 21 2006
Days 4-8 no
risk of high-end severe storms
updated 1446 UTC April 17 2006
Weak wsw mid to high level flow will persist ahead of an upper trough through April 18. Widespread
storms will occur across Bengal. These storms will not be tornadic and will not contain extremely large
hail WSW mid to high level flow is not conducive to high-end severe storms. However, by April 19
and 20, the flow will become more westerly in the base of the trough, albeit not very strong. There will
be a slight chance for high-end severe storms on these days.
I am on vacation through April 24 so updates will be
few and far between.
Storms
were still raging as of 1438 UTC.
Well, get ready for another day of
severe storms. I suspect based on the surface observations
The warm sector has been shunted into
southern Bangladesh with light winds across the country.
The 06 UTC surface
map showed a wnw to ese oriented trough and a dryline in its familiar
position. Storms will
The 00 UTC surface
chart shows 3 distince boundaries. A dryline was in its climatological
position. An outflow
Wow, there was actually a sounding from Dhaka
this morning. This shows a convective temperature of about 90F.
Major tornadoes usually do not occur in the entrance region of a jet
in Bangladesh. The surface pattern tends to be
A tornado watch will be required by 6 UTC (noon) for much of central
and southern Bangladesh.
UK initialization for April 5 can be found here. The 09
UTC surface chart is here. The aqua MODIS pass was way late but is
now
The 00z UKMET shows the high level jet core near or just north of Meghalaya,
India. The outflow boundary
700 29035kt
Storms
rolled across northeast Bangladesh this morning leaving an outflow boundary.
These storms had exited
The surface flow will be southerly except easterly just north of the
outflow boundary. Given the convergence
updated
1340 UTC April 11 2006
The
flow will be fairly weak at mid levels and the high level jet will be north
of Bengal through April 14.
In fact, the mid to high level flow will become more west-southwesterly
by April 15 and 16. This may
preclude high-end severe storms through April 19.
updated
1358 UTC April 08 2006
Storms
exploded between
2 and 3 pm again
today. 9
UTC sfc map is here. 12UTC
surface map.
updated
0413 UTC April 08 2006
A tornado watch has been issued for
much of Bangladesh until 9 pm local time.
Watch graphics will not be posted
today as the author of this page needs a decent
nights sleep. :)
updated
0330 UTC April 08 2006
Supercell storms are likely again
today with 40+ kt flow at 500mb and 50-60kt high level flow.
This will be the last day of high-end
storms for a while. The high level jet will retreat north of the
region withweak flow over Bengal.
updated
1319 UTC April 07 2006
updated
1319 UTC April 07 2006
updated
1000 UTC April 07 2006
updated
0656 UTC April 07 2006
that the day will unfold similar to yesterday, with storms exploding near
or north of Ishurdi
just east of the dryline/front intersection and possiblynorth
and northwest of Dhaka along
the surface boundary.
central Bangladesh until 9 pm local time.The
mainthing that will distinguish
another day
of supercell storms, from the majortornadic
storms is the strength of the low level inflow.
The 00 UTC sounding
from Agartala, IN(60 east of Dhaka) can be found here.
updated
0532 UTC April 07 2006
60kt(300mb) to 80kt(200mb) high
level flow will continue today with continued strong flow at 500mb
(40-50kts). Themain forecast
problem is how much airmass recovery will occur and what boundaries
willfocus convection. Stay
tuned to the 07z update once I look at the 06 UTC observations.
updated
1154 UTC April 06 2006
A
storm
has exploded
in western Bangladesh near Ishurdi. The 9 UTC surface map is here.
updated
0715 UTC April 06 2006
likely develop near Ishurdi(west-central BD over the next 2 hours.
Therefore a TORNADO
WATCH has been
issued for much of central Bangladesh until 9 pm local time.
updated
0225 UTC April 06 2006
Bangladesh will be in the entrance
region of the jet today as shown by the 18hr UKMET 250mb fcst valid
12 UTC April 6 2006 as a weak
shortwave trough undercuts the Tibetan Plateau. Vertical wind shear
will
be quite good with 40kts at 700,
50 kts at 500mb
and 80 kts at 250mb, along with southerly winds at the surface.
There is an outflow boundary across
central Bangladesh which will serve as a focus for storms. Isolated storms
may also form on the dryline and at
the intersection of the dryline and the wnw-ese oriented trough.
boundary was further south than in
previous days and the wnw-ese oriented trough was in its familiar position.
T/TD of 90F/75F would give a lifted index of -10 which of course is
extremely unstable. The low levels have been
worked over by convection but this will quickly change. I am
not sure where the boundary will end up this
afternoon, but probably just south of Dhaka??
less robust with weaker surface winds??? This is just speculation.
Storms
were continuing
across central Bangladesh even at 1438
UTC.
updated
1045 UTC April 05 2006
available. 1
km
Towering cumulus clouds could be seen
along the dryline. The outflow boundary is clearly visible
with stable stratocu to the north and
cumuliform clouds to the south.
updated
0930 UTC April 05 2006
Storms are erupting
about 20 to 30 miles north and northwest of Dhaka. These storms will quickly
become severe. The 20 million people
that live in Dhaka could be impacted by these storms.
The Zmax
showed a storm developing off the dryline to the southwest of Calcutta
as well as the
storms north of Dhaka.
updated
0635 UTC April 05 2006
A
tornado
watch has been issued for much of central and northern Bangladesh until
9 pm local time.
An outflow boundary from morning thunderstorms will be the focus for
new storms. Initiation
will probably be near Jamalpur, Mymensingh or Siraganj by mid afternoon.
The storms will then
move SE toward Dhaka and Agartala toward evening.
updated
0635 UTC April 05 2006
We are in luck today. There will be
an aqua MODIS (polar orbiting) pass at 0730 UTC near 26N, 88E
with 250m resolution. This may showa
festering cu field and any boundaries that may lead to storms. I
will use this to help in decision making about a tornado watch.
was located from 24 to 25N. The wind field will look like the following:
500 29050kt
300 29080kt
200 29085kt
Bangladesh as of 0238 UTC leaving an outflow
boundary behind. The 06 UTC surface map shows this boundary.
along the boundary, storms will probably develop despite the jet being
just north. A tornado watch will be issued
shortly.
updated
0548 UTC April 05 2006
The high level jet core is located
across far northern Bengal today. The best chance of severe
would be north of 25N. But will
the airmass recover that far north? The 6 UTC surface obs
and the hourly observations from Dhaka-Kurmitola will be key.
500mb chart 00 UTC 4 April 2006
updated 1240 UTC April 04 2006Explosive thunderstorm development
is immiment. A stationary frontal
boundary(noon map) and dryline
will be thefocus for storms.
Intitial development will be in fat east India or western Bangladesh where
the
drylineintersects the boundary.
Thus a tornado
watch has been issued for central and southern Bangladesh
and extreme east India. The 0538Z
radar image from Calcutta shows a few leftover storms around Dhaka,
which were serving to reinforce the outflow boundary.
For upper level charts for yesterdays
severe storm outbreak, go here. I used the 12 hr
UKMET
as the initialization.
Storms are still going at 1138
UTC.
Explosive
thunderstorm development has occurred over the past 2 hours. Several
supercell storms
are now in progress.
An isolated
cell is developing west of Rajshahi. This cell is on the edge of the
tornado watch but will
move southeast into the watch area. The PDS
has been shifted further west.
The latest Terra MODIS pass over Myanmar
at
0425 UTC confirms my initial analysis of an
Calcutta radar 0530
UTC.
outflow boundary over central
Bangladesh. Explosive thunderstorm development should occur
between 9 UTC and 11 UTC.
Unfortunately, there is no sounding information in the Bengal region
today which makes forecasting
even more of a challenge. It appears that the most likely place for
storm initiation is western
Bangladesh along the outflow boundary and just east of the dryline.
In other words, storm will
likely develop just ahead of the dryline/outflow boundary intersection.
or along the west-east oriented
trough. Thus the tornado watch has been upgraded to a
PDS(particularly
dangerous situation) for much of central Bangladesh.
A
tornado watch has been issued for much of central and northern Bangladesh andDiscussion: updated 0150 UTC April 03 2006
A supercell
storm developed in west central Bangladesh about 4 pm(10 UTC on April
2).
The 12z
surface map showed an intersection of a dryline and trough in far east
India.
The approximate
sounding for the area showed a lifted index of -11. This is modified
from the upstream Patna
sounding.
An outflow
boundary has been generated by widespread nocturnal storms over
northern and central Bangladesh.
Thunderstorms will explode near the intersection of
this outflow boundary(if
it remains intact) and the dryline. If the outflow boundary
does not remain intact,
then the trough/dryline intersection would be the initiation
point.
By 12
UTC April 3, the exit region of a jet streak will be nosing into Bangladesh.
This is the prototypical
example. This will
help increase the low level flow into Bangladesh, thus leading to a favorable
shear
profile for tornadoes.
With increasing flow at all
levels, any storms that develop today could produce extremely large
hail and violent tornadoes.
Surface dewpoints should be even higher today then yesterday
which will result in lower
cloud bases and even higher instability.
Discussion: updated 0500 UTC March 30 2006
My composite reanalysis for 62 Bengal tornado cases
can be found here.
Note that tornadoes tend to
occur when the exit region of the high level jet
is over Bengal.
ECMWF
day 5 200mb and 500mb from 12 UTC March 29 and valid at 12 UTC April 03
2006
ECMWF
day 7 200mb and 500mb from 12 UTC March 29 and valid at 12 UTC April 05
2006
GFS
114hr 500mb hgt and sfc wind from 18 UTC March 29 and valid at 12 UTC April
03 2006
GFS
138hr 500mb hgt and sfc wind from 18 UTC March 29 and valid at 12 UTC April
04 2006
GFS
162hr 500mb hgt and sfc wind from 18 UTC March 29 and valid at 12 UTC April
05 2006
ECMWF
day 5 SLP and 500hgt from 12 UTC March 29 and valid at 12 UTC April 03
2006
ECMWF
day 6 SLP and 500hgt from 12 UTC March 29 and valid at 12 UTC April 04
2006
ECMWF
day 7 SLP and 500hgt from 12 UTC March 29 and valid at 12 UTC April 05
2006
The climatological tornado peak is April
10-14. There is a sharp decline in violent tornadoes after April
19. There have
been a few notable tornadoes in May. However, 2
of the most violent tornadoes on record occurred outside of the peak
period on April 26 and May 13, with 1300 and 700
fatalities respectively. The April 26th tornado path was 8 miles long
but up to a mile wide. Interestingly, the violent
tornado on March 20, 2005 that killed 65 people was very early. Very
few violent tornadoes have occurred so early in
the spring. The exceptions were March 19, 1961 when over 200
people were killed by a single tornado and March
13, 1953 when over 20 were killed. Only 2 violent tornadoes have
occurred after May 13.
Several factors lead to a very short
but active severe weather season across Bengal.
North and central India
heats
up and dries out in late March or early April. A deep, dry mixed
layer develops.
Low
level flow from the Bay of Bengal increases markedly during this
time.
Westerly mid-level flow around
the Tibetan Plateau advects the Indian mixed layer over
the Bengal moist tongue.
This leads to the elevated
mixed layer. Note that parts of the Indian
desert are "elevated"(1-3000ft)
compared to Bangladesh which is near sea level.
The mid level flow is still
fairly strong in April with 30-50kt 700mb flow and 35 to 50 kt 500mb
flow fairly common.
The high level jet is usually over or just north of the Bengal in April.
The southern branch of the
polar jet often retreats north of the Tibetan Plateau by May,
leaving
light mid to high level
flow across the Bengal region. By June
the high level flow is light.
All these factors result in a tornado maximum in early
to mid April. In short, vertical wind shear
and instability are maximized
and the jet is in a favorable position during this time.
Severe storms or tornado hits Bangladesh killing over 20
Over 20 people have been killed in a tornado or severe thunderstorm on May 17, 2005.
Bangladeshi picking up hail
stones on April 25, 2005. This picture appeared in the "Daily Sangram".
Tornado hits northern Bangladesh killing 65
A tornado
killed at least 65 people in northern Bangladesh on Sunday March 20, 2005.
This tornado hit Sadullahpur and Sudarganj
upazilas of Gaibandha and Mithapukur upazila of
Rangpur. I am currently preparing a case
study with surface and upper air charts.
On March 18, before leaving town on a 2 day trip,
I issued a slight risk for March 19 and the first moderate risk of the
year
for March 20. Unfortunately, I apparently overwrote
this file by mistake since I cannot find the March 20 forecast showing
the
moderate risk.
High
winds and lightning killed 7 people
in scattered locations across Bangladesh on March 30, 2005.
Thunderstorm winds and lightning kill
20
Storms developed on March 23, 2005 in a tornado
watch. At least 16
people were killed across Bangladesh. The deaths were
scattered in nature and were the result of strong
straight line winds and lightning. Lightning killed 4 people working in
a field.
An outflow
boundary can be seen on the 06 UTC Mar 23 surface map. Surface
dewpoints south of this boundary were in the
mid to upper 70s(24 to 25C) and surface based lifted
indices ranged from -9 to -12 along and south of this boundary. Some of
these deaths may have been from storms on March
22.
A jet streak was approaching Bengal as seen from
the UKMET 250mb initialization.
The 500mb
chart at 12 UTC March 23
showed a shortwave trough over western India. I
analyzed this map despite the very poor data quality over India, and the
paucity
of upstream data. The large
view and small
view 12UTC March 23 UKMET initialization 500mb maps are also
available.
8 people were killed by lightning in 4 separate cases in India over the past few days(March 19-23, 2005).
A late evening thunderstorm on Marh 19, 2005 killed
a couple on the western end of the Khasi Hills in the Meghalaya
state of India.
Morning(6am BST) soundings from Dhaka--good
job BMD(Bangladesh Meteorological Department). These are
high quality soundings(especially the T/Td data)--a
dramatic improvement from years past. These are from April 2004.
A tornado
hit in northern Bangladesh on April 14, 2004, killing 75 people.
Click here
for details about the tornado in far eastern Bangladesh on May 4, 2003.