SHAMSUDDIN AHMEDSHAMSUDDIN AHMEDASSISTANT DIRECTORASSISTANT DIRECTOR

BANGLADESH METEOROLOGICAL BANGLADESH METEOROLOGICAL DEPARTMENTDEPARTMENT

The Thirty-eight session of The Thirty-eight session of WMO/ESCAP Panel on Tropical WMO/ESCAP Panel on Tropical

Cyclones (New Delhi, India, Cyclones (New Delhi, India, 21-26 February, 2011)21-26 February, 2011)

Country Report on Country Report on 2010 2010

Cyclone SeasonCyclone Season

BangladeshBangladesh

Cyclonic Storm ‘Laila’ over North Cyclonic Storm ‘Laila’ over North Bay during 17-20 May 2010 Bay during 17-20 May 2010

A low formed over Andaman Sea and adjoining A low formed over Andaman Sea and adjoining Southeast Bay at 0600UTC of 16 May 2010. Then it Southeast Bay at 0600UTC of 16 May 2010. Then it moved west-northwestwards and intensified into a moved west-northwestwards and intensified into a well-marked low over Southeast Bay and adjoining well-marked low over Southeast Bay and adjoining area on 17 May 2010. The system further intensified area on 17 May 2010. The system further intensified into Depression at 0900UTC of 17 May 2010 over into Depression at 0900UTC of 17 May 2010 over the same area. Then it moved northwestwards and the same area. Then it moved northwestwards and again intensified in a Deep Depression over same again intensified in a Deep Depression over same area at 1500UTC of same day. area at 1500UTC of same day.

Cyclonic Storm Cyclonic Storm ‘‘LailaLaila’’ over over North Bay during 17-20 North Bay during 17-20

May 2010 May 2010

After that it moved almost northwestwards and After that it moved almost northwestwards and intensified further into a cyclonic storm ‘Laila’ over intensified further into a cyclonic storm ‘Laila’ over the same area at 0000 UTC of 18 May 2010. Then it the same area at 0000 UTC of 18 May 2010. Then it moved continuously northwestwards and finally moved continuously northwestwards and finally crossed northeast Andhra Coast of India near crossed northeast Andhra Coast of India near Machalipatnum in the afternoon (at about 1200UTC) Machalipatnum in the afternoon (at about 1200UTC) of 20 May 2010 and lay over Bapatla and adjoining of 20 May 2010 and lay over Bapatla and adjoining area and weakened afterwards. The track of the area and weakened afterwards. The track of the cyclonic storm ‘Laila’ is illustrated in Fig. 1.cyclonic storm ‘Laila’ is illustrated in Fig. 1.

Figure 1: BMD observed track of cyclonic storm ‘Laila’ during 17-20 May 201017-20 May 2010 .

Depression over west central Depression over west central Bay 7-8 October 2010Bay 7-8 October 2010

A low formed over West Central Bay and adjoining A low formed over West Central Bay and adjoining North Bay in the morning of 07 October 2010 and North Bay in the morning of 07 October 2010 and concentrated into a Depression (with central position concentrated into a Depression (with central position 17.0°N and long 85.0°E) at 0900UTC of same day. 17.0°N and long 85.0°E) at 0900UTC of same day. The system moved initially northwards and recurved The system moved initially northwards and recurved towards West Bengal-Bangladesh Coast them to towards West Bengal-Bangladesh Coast them to Bangladesh coast. Finally it crossed Khulna-Barisal Bangladesh coast. Finally it crossed Khulna-Barisal coast of Bangladesh coast near Mongla in the coast of Bangladesh coast near Mongla in the morning of on 08 October 2010. The track of the morning of on 08 October 2010. The track of the depression is given in Fig. 2. depression is given in Fig. 2.

Fig. 2: BMD observed track of Depression during 07-08 October 2010.

Depression over North Bay during Depression over North Bay during 13-15 October 2010 13-15 October 2010

A low formed over East Central Bay and adjoining area A low formed over East Central Bay and adjoining area on 12 October 2010. On 13 October the system on 12 October 2010. On 13 October the system intensified into a well-marked low over the same area. intensified into a well-marked low over the same area. Then the system moved northwestwards and Then the system moved northwestwards and intensified into a depression at 0000UTC of 13 October intensified into a depression at 0000UTC of 13 October and deep depression at 0000UTC of 14 October 2010 and deep depression at 0000UTC of 14 October 2010 over East Central Bay and adjoining West Central Bay over East Central Bay and adjoining West Central Bay and North Bay. After that it moved continuously and North Bay. After that it moved continuously northwestwards and crossed Orissa coast near northwestwards and crossed Orissa coast near Gopalpur (India) at 2100UTC of 15 October 2010 andGopalpur (India) at 2100UTC of 15 October 2010 and

Depression over North Bay during Depression over North Bay during 13-15 October 2010 13-15 October 2010

located over Orissa and adjoining area as a land located over Orissa and adjoining area as a land depression. After that the system moved depression. After that the system moved northwestwards, weakened gradually by giving northwestwards, weakened gradually by giving precipitation and became unimportant. The track of precipitation and became unimportant. The track of the Deep Depression is illustrated in Fig. 3. During the the Deep Depression is illustrated in Fig. 3. During the life time of Deep Depression steep pressure gradient life time of Deep Depression steep pressure gradient persists over North Bay and deep convection was persists over North Bay and deep convection was taking place. Therefore high wind and heavy rainfall taking place. Therefore high wind and heavy rainfall were recorded in the coastal districts of Bangladesh. were recorded in the coastal districts of Bangladesh.

Fig. 3: BMD observed track of Depression during 13-15 October 2010.

A low formed over north Andaman Sea and adjoining East Central Bay on 18 October 2010. Then it moved northwestwards over East Central Bay and adjoining area and intensified into a well-marked low. After that the system moved slightly northwards and concentrated into a depression over East Central Bay and adjoining Northeast Bay at 1800UTC of 20 October 2010. At 0600UTC of 21October 2010, the system intensified further into a Deep Depression over the same area. At 0900UTC of same day the system again intensified into a cyclonic storm ‘GIRI’ over North Bay and adjoining East Central Bay and moved

Cyclonic Storm ‘GIRI’ over North Bay during 20-22 October 2010

north-northeastwards. At 0600UTC and 1100UTC of 22 October the system further intensified into a severe cyclonic storm ‘GIRI’ and severe cyclonic storm with a core of hurricane winds ‘GIRI’ respectively. At about 1400UTC of 22 October, the system started to cross Myanmar Coast (south of Sittwe) and completed crossing the coast during next 3-4 hours and weakened afterwards. During this period gusty winds were recorded in the southeastern parts of Bangladesh and no casualties were reported. The track of the severe cyclonic storm ‘GIRI’ is illustrated in Fig. 4.

Cyclonic Storm ‘GIRI’ over North Bay during 20-22 October 2010

BMD observed track of severe cyclonic Storm ‘GIRI’ during 20-22 October 2010 of cyclone ‘GIRI’ October 2010

A low formed over south Andaman Sea and adjoining area on 02 November 2010, moved westwards and concentrated into a depression at 0600UTC of 04 November 2010. Then the system moved mainly westwards into Southwest Bay and adjoining areas and intensified into deep depression at 0300UTC of 05 November 2010. At 0600UTC of same day the system intensified into a cyclonic storm ‘Jal’ over the same area. Moving continuously towards west-northwesterly or northwesterly direction the system further intensified into a severe cyclonic storm ‘Jal’ at 0000UTC of 06 2010 over Southwest Bay and adjoining Southeast Bay.

Cyclone ‘Jal’ during 04-07 November 2010

November After that it moved northwestwards to November After that it moved northwestwards to Tamilnadu coast of India over Southwest Bay but Tamilnadu coast of India over Southwest Bay but remained practically stationary for sometime on the remained practically stationary for sometime on the way of its movement. But at 0900UTC of 07 way of its movement. But at 0900UTC of 07 November 2010 when it was slightly away from the November 2010 when it was slightly away from the Tamilnadu coast of India, the system weakened into a Tamilnadu coast of India, the system weakened into a cyclonic storm ‘Jal’ as it lost it energy by giving high cyclonic storm ‘Jal’ as it lost it energy by giving high amount precipitation. After that system started to amount precipitation. After that system started to cross north Tamilnadu coast of India and by midnight cross north Tamilnadu coast of India and by midnight of same day it crossed Tamilnadu coast of India near of same day it crossed Tamilnadu coast of India near Chennai. The observed path of the cyclonic storm Chennai. The observed path of the cyclonic storm ‘Jal’ is illustrated in fig 5‘Jal’ is illustrated in fig 5

Cyclone ‘Jal’ during 04-07 November 2010

Fig. 5: BMD observed track of cyclone ‘Jal’ during 04-07 November 2010

There was no tropical cyclone directly affecting Bangladesh. A There was no tropical cyclone directly affecting Bangladesh. A

Depression over North Bay during 07-08 October 2010 that crossed Depression over North Bay during 07-08 October 2010 that crossed

Khulna-Barisal coast of Bangladesh near Mongla in the morning of Khulna-Barisal coast of Bangladesh near Mongla in the morning of

on 08 October 2010. Because of the Deep Depression over North on 08 October 2010. Because of the Deep Depression over North

Bay during 13-15 October 2010 that crossed Orissa coast near Bay during 13-15 October 2010 that crossed Orissa coast near

Gopalpur (India), Steep pressure gradient persists over North Bay Gopalpur (India), Steep pressure gradient persists over North Bay

and deep convection was taking place. Therefore high wind and and deep convection was taking place. Therefore high wind and

heavy rainfall were recorded in the coastal districts of Bangladesh. heavy rainfall were recorded in the coastal districts of Bangladesh.

Local Cautionary Signal No. III were also advised to hoist for the Local Cautionary Signal No. III were also advised to hoist for the

maritime ports and fishing boats & trawlers over North Bay and maritime ports and fishing boats & trawlers over North Bay and

Deep Sea during this period as a precautionary measure. Deep Sea during this period as a precautionary measure.

Report On The Impact Of Tropical Cyclones

Meteorological componentMeteorological component

Meteorological Data from RTH New Delhi and 10 synoptic Meteorological Data from RTH New Delhi and 10 synoptic observatories of BMD are exchanged on routine basis through observatories of BMD are exchanged on routine basis through WMO’s GTS. All the 35 observatories of BMD have been WMO’s GTS. All the 35 observatories of BMD have been connected with NMCC Dhaka either by TP or Telephone and connected with NMCC Dhaka either by TP or Telephone and single sideband (SSB) etc. or by all the three systems. Some of single sideband (SSB) etc. or by all the three systems. Some of the observatories are connected through internet with NMCC and the observatories are connected through internet with NMCC and data are collected on real time basis by using Meteorological data are collected on real time basis by using Meteorological Data Acquisition software. The communications between Storm Data Acquisition software. The communications between Storm Warning Centre (SWC) and Radar Station at Cox’s Bazar and Warning Centre (SWC) and Radar Station at Cox’s Bazar and Khepupara have been upgraded to VSAT link. NMCC uses MSS Khepupara have been upgraded to VSAT link. NMCC uses MSS software obtained from WMO/UNDP Regional Computer Network software obtained from WMO/UNDP Regional Computer Network programme for reception and transmission of all meteorological programme for reception and transmission of all meteorological data.data.

Bangladesh Meteorological Department has been Bangladesh Meteorological Department has been using JMA Global Spectral Model (GSM) for using JMA Global Spectral Model (GSM) for Numerical Weather Prediction since October Numerical Weather Prediction since October 2010. The resolution for the surface is 0.252010. The resolution for the surface is 0.25°°x0.25x0.25°° and for upper air is 0.5and for upper air is 0.5°°x0.5x0.5°°. The model out are . The model out are updated everyday accordingly at BMD’s website updated everyday accordingly at BMD’s website www.bmd.gov.bdwww.bmd.gov.bd

Meteorological componentMeteorological component

Hydrological ComponentHydrological Component

Bangladesh Meteorological Department provides all Bangladesh Meteorological Department provides all sorts of data, information and weather forecast to sorts of data, information and weather forecast to the Flood Forecasting and Warning Centre (FFWC) the Flood Forecasting and Warning Centre (FFWC) of Bangladesh Water Development Board (BWDB). of Bangladesh Water Development Board (BWDB). A Metropolitan Area Network (MAN) between SWC, A Metropolitan Area Network (MAN) between SWC, Dhaka and FFWC was established in 1998 through Dhaka and FFWC was established in 1998 through which FFWC receives meteorological and which FFWC receives meteorological and hydrological data (including rainfall and water hydrological data (including rainfall and water discharge data of up stream) along with Radar and discharge data of up stream) along with Radar and Satellite images. Satellite images.

Through the completion of the establishment of Meteorological Through the completion of the establishment of Meteorological and Hydrological Doppler Radar at the north-eastern part of and Hydrological Doppler Radar at the north-eastern part of Bangladesh under JICA Grant Assistance, FFWC is being Bangladesh under JICA Grant Assistance, FFWC is being connected by VSAT link to get all the radar information for flood connected by VSAT link to get all the radar information for flood and flash flood monitoring and forecasting. Also during and flash flood monitoring and forecasting. Also during execution of JICA’s Technical Cooperation on the Human execution of JICA’s Technical Cooperation on the Human Capacity Development training will be imparted to FFWC for Capacity Development training will be imparted to FFWC for radar data calibration and its utilization.radar data calibration and its utilization.

Hydrological ComponentHydrological Component

Disaster prevention and preparedness Disaster prevention and preparedness componentcomponent

Bangladesh is most vulnerable to recurring natural disasters including cyclone and the associated storm surge. These particular disasters are known to disrupt people’s lives, livelihood, and devastable development momentum in some part of the country. Over the past few years, climate change has added significant perturbation in the hydrological cycle and increased the frequency and intensity of the hydro-meteorological disasters such as the cyclones. This reaches to the extent where the international community has placed Bangladesh as the worst victim of climate-induced disaster.

Disaster prevention and preparedness Disaster prevention and preparedness componentcomponent

In view of the cyclone season, the government intends to implement the provisions of the National plan for disaster Management, 2010 (Section 10: Disaster Management Regulatory Framework, section 11: Disaster Management plans, and Dtanding order on Disaster, 2010 ) in the form of Response Plan for Cyclone Season. This response plan aims at eliminating or mitigating the cyclone risk by understaking coordinated activities for the prevention of, preparation for, response to and recoveries from the impact of cyclone.

Training ComponentTraining Component

Mr. Md. Abdul Mannan, & Mr. Md. Nurul Karim, Meteorologist, participated in the “ICTP Targeted Training activity: statistical methods in seasonal prediction” at ICTP, Italy from 02-13 August 2010

Mr. Md. Hafizur Rahman, Meteorologist, participated in the “seventh post graduate Course in Satellite Meteorology and Global Climate (SATMET-7)” at Ahmedabad, India from 01 August 2010-30 April 2011.

Mr. Md. Shameem Hassan Bhuiyan, Meteorologist, participated in the “USDA Cochran fellowship program” at USA, from 25 October - 02 November 2010.

Ms. Arjumand Habib, Director, participated in the “GEO-VII plenary meeting and 2010 GEO ministerial summit” at Beijing, China from 03-05 November 2010.

Mr. Shamsuddin Ahmed, AD, participated in the “Challenge Programme on Climate, agriculture and development priorities and scenario development workshop” at New Delhi, India from 08-10 November 2010

Research/Publication ActivitiesResearch/Publication Activities

Research studies have been carried out in the following topics by the members of the Department-

Analysis of extreme rainfall events

Analysis of Tropical cyclone “AILA”.

Analysis of significant Nor‘wester events

BMD provides information on significant weather and new developments related to meteorology through BMD’s newsletters