WTIN20 DEMS 311825
DEMS-RSMC SPECIAL TROPICAL CYCLONES NEW DELHI DATED 31.10.2026
SPECIAL TROPICAL WEATHER OUTLOOK FOR THE NORTH INDIAN OCEAN (THE BAY
OF BENGAL AND THE ARABIAN SEA) VALID FOR THE NEXT 168 HOURS ISSUED AT
1800 UTC OF 31.10.2026 BASED ON 1200 UTC OF 31.10.2026.
SUB: DEPRESSION OVER SOUTHEAST BAY OF BENGAL
THE DEPRESSION OVER SOUTHEAST BAY OF BENGAL AND ADJOINING AREAS OF
ANDAMAN & NICOBAR
ISLANDS AND ANDAMAN SEA MOVED WEST-NORTHWESTWARDS WITH SPEED OF 30
KMPH DURING PAST 6
HOURS AND LAY CENTERED AT 1200 UTC OF TODAY, THE 31ST OCTOBER, 2026
OVER SOUTHEAST BAY OF
BENGAL, NEAR LATITUDE 10.5ON AND LONGITUDE 88.6OE, ABOUT 960 KM
EAST-SOUTHEAST OF CHENNAI
(CHENNAI, 43279), 980 KM SOUTHEAST OF VISHAKHAPATNAM (ANDHRA PRADESH,
43149) AND 1030 KM
SOUTHEAST OF MACHILIPATNAM (ANDHRA PRADESH, 43185) AND 1080 KM
EAST-SOUTHEAST OF ONGOLE
(ANDHRA PRADESH, 43221).
IT IS VERY LIKELY TO MOVE WEST-NORTHWESTWARDS AND INTENSIFY INTO A
DEEP DEPRESSION OVER
SOUTHEAST BAY OF BENGAL BY 1800 UTC OF TODAY, INTO A CYCLONIC STORM
OVER THE SAME REGION ON
1ST NOVEMBER AND INTO A SEVERE CYCLONIC STORM OVER WESTCENTRAL BAY OF
BENGAL ON 2ND
NOVEMBER.
IT IS VERY LIKELY TO REACH OVER WESTCENTRAL BAY OF BENGAL NEAR SOUTH
ANDHRA PRADESH COAST 2100
UTC OF 3RD NOVEMBER AND CROSS SOUTH ANDHRA PRADESH COAST AS A SEVERE
CYCLONIC STORM WITH
WIND SPEED OF 100 TO 110 KMPH GUSTING 120KMPH BETWEEN NELLORE AND
NARSAPUR BY 0300 UTC
OF 3RD NOVEMBER 2026.
FORECAST LOCATION AND INTENSITY ARE GIVEN IN FOLLOWING TABLE:
DATE/TIME     POSITION              MAXIMUM SUSTAINED SURFACE
CATEGORY OF CYCLONIC
  (IST)      (LAT. 0N/ LONG. 0E)     WIND SPEED (KMPH)
DISTURBANCE


31.10.26/1230 10.5/88.6              45-55 GUSTING   TO 65
DEPRESSION
31.10.26/1830 10.9/88.2              50-60 GUSTING   TO 70       DEEP
DEPRESSION
01.10.26/0530 11.3/87.3              60-70 GUSTING   TO 80
CYCLONIC STORM
01.11.26/1130 11.8/86.3              65-75 GUSTING   TO 85
CYCLONIC STORM
01.11.26/1730 12.3/85.4              70-80 GUSTING   TO 90
CYCLONIC STORM
02.11.26/0530 13.2/83.4              80-90 GUSTING   TO 100
CYCLONIC STORM
02.11.26/1730 14.3/81.6              90-100 GUSTING  TO 110
SEVERE CYCLONIC STORM
03.11.26/0530 15.4/80.3              100-110 GUSTING TO 120
SEVERE CYCLONIC STORM
03.11.26/1730 16.6/79.2              70-80 GUSTING   TO 90
CYCLONIC STORM
04.11.26/0530 17.9/78.1              50-60 GUSTING   TO 70       DEEP
DEPRESSION
04.11.26/0530 19.3/77.3              35-45 GUSTING   TO 55
DEPRESSION

THE ESTIMATED CENTRAL PRESSURE IS 1008 HPA AND MAXIMUM SUSTAINED WIND
SPEED IS 25 KT
GUSTING TO 35KT.
A BUOY NEAR 15.6ON/88.0OE REPORTED MSLP OF 1015.0 HPA AND MSW 800

(WIND DIRECTION)/10.0KT,

ANOTHER, BUOY NEAR 6.0N/90.3E REPORTED MSLP OF 1014.0 AND MSW 240
0
(WIND DIRECTION)/10.0KT.

HATBAY (43364) REPORTED MSLP OF 1012.2 HPA AND MSW 230
0
(WIND DIRECTION)/1.0KT, AND

MAYABANDAR (43309) REPORTED MSLP OF 1013.1 HPA AND MSW 50
0
(WIND DIRECTION)/2.0KT

AS PER LATEST INSAT 3DS IMAGERY BASED ON 1200 UTC VORTEX OVER
SOUTHEAST BAY OF BENGAL AND
NEIGHBOURHOOD CENTRED NEAR 10.3N / 88.5E INETENSITY T1.5.
SPIRAL BANS ARE APPEARING THE CLOUD IMAGING INDICATE SHEAR TO
NORTHWEST, FURTHER THE SPIRAL BANDS
ALSO APPEARING IN THE NORTHERN SECTOR. THE CLOUD SHOWS GRADUAL
ORGANIZING DURING PAST 12 HOURS.
ASSOCIATED SCATTERED TO BROKEN LOW/MEDIUM CLOUDS WITH EMBEDDED
INTENSE TO VERY INTENSE
CONVECTION OVER SOUTHEAST ADJACENT TO CENTRAL BAY OF BENGAL , ANDAMAN
& NICOBAR ISLANDS WITH
MINIMUM CTT -70OC TO -90OC.
BASED ON HYSAT 008UTC AND OCEANSAT BASED ON 0706 UTC SCRATEROMETER
BASED WINDS
INDICATES AN STRONGER INDICATE NORTHEAST & ADJOIN SOUTHEAST SECTOR
WITH SPEED REACHING 25-35
KTS. IT IS 25-35 KTS IN NORTHWEST SECTOR AND 10-15 KTS IN SOUTHWEST
SECTOR.
REMARKS:
SEA SURFACE TEMPERATURE IS AROUND 290C OVER ANDAMAN SEA AND ENTIRE
BOB. IT HAS REDUCED BY 10C OVER
THE REGION COMPARED TO LAST WEEK. THE OCEAN HEAT CONTENT IS 60-70
KJ/CM2

COMPARED TO 100 KJ/CM2
DURING VERY SEVERE CYCLONIC STORM \U2018ARNAB\U2019. THE MADDEN
JULIAN OSCILLATION (MJO) IS CURRENTLY IN PHASE 3
WITH AMPLITUDE MORE THAN 1. IT IS LIKELY TO CONTINUE IN SAME PHASE
DURING THE ENTIRE FORECAST PERIOD WITH
AMPLITUDE MORE THAN 1. THE GUIDANCE FROM THE NCICS MODEL INDICATES
THE PREVALENCE OF WESTERLY WIND
ANOMALY (>9 MPS) ALONGWITH MJO OVER SOUTH BAY OF BENGAL AND SOUTH
ANDAMAN SEA AND EASTERLY WIND
ANOMALY (>9 MPS) ALONGWITH KELVIN WAVE (KW) TO ITS NORTH OVER NORTH
BOB AND ADJOINING AREAS OF
EASTCENTRAL BOB. PREVALENCE OF KELVIN WAVE IN THE NORTHERN PARTS OF
BOB WILL ENHANCE EXTRA-TROPICAL
WESTERLIES OVER THE NORTH BOB. IT WILL BRING COLD AND DRY AIR FROM
NORTHWEST OVER THE REGION, WHICH IS NOT
SUPPORTIVE FOR HIGHER INTENSIFICATION OF THE SYSTEM. HOWEVER AT THE
SAME TIME, ACTIVE MJO PHASE IS
PERSISTING OVER THE REGION WHICH WILL ENHANCE CONVECTIVE ACTIVITY AND
HENCE INTENSIFICATION OF DEPRESSION
OVER BOB.
VARIOUS ENVIRONMENTAL FEATURES INDICATES, THE POSITIVE LOW-LEVEL
VORTICITY AT 850 HPA HAS INCREASED DURING
PAST 24 HOURS AND IS AROUND 100 X10-6
S
-1
OVER SYSTEM AREA WITH VERTICAL EXTENSION UP TO 500 HPA. THE LOW

LEVEL CONVERGENCE IS THE SAME IN PAST 24 HOURS AND IS AROUND 5 X10-6
S
-1
OVER SYSTEM AREA. UPPER-LEVEL

DIVERGENCE HAS INCREASED IN PAST 24 HOURS AND IS AROUND 20X10-6
S
-1

OVER SYSTEM AREA. MID-LEVEL WIND-
SHEAR (500-850 HPA) IS LOW (5-10 KT) AROUND THE SYSTEM CENTRE. THE
AREA OF MAXIMUM CONVERGENCE AND

DIVERGENCE SUPERIMPOSED WITH EACH OTHER. THE MID-LEVEL WIND-SHARE,
WHILE IT IS ANTICLOCKWISE IMMEDIATELY
NEAR THE SYSTEM CENTER (UPTO 85OE) IT BECOME CLOCKWISE OVER SOUTHWEST
WEST CENTRAL BAY OF BENGAL, HENCE
SUCH TYPE OF SHEAR WILL SUPPORT INTENSIFICATION WHILE THE SYSTEM WILL
MOVING TOWARDS THE COAST, AFTER REACHING
85N. THE RATE OF INTENSIFICATION MAY INCREASE FROM 1ST NOVEMBER
EVENING DUE TO SUCH SUPPORTIVE WIND
SHEAR.
THE HIGH-LEVEL WIND SHEAR IS ALSO LOW TO MODERATE AROUND THE SYSTEM
CENTRE AND ALONG THE FORECAST TRACK.
THE ANTI-CYCLONIC SHEAR PREVAILS OVER THE ENTIRE AREA OF SOUTH AND
CENTRAL BAY OF BENGAL AND ALONG SOUTH
PENINSULAR WHICH IS SUPPORT INTENSIFICATION OF THE SYSTEM.

AN UPPER TROPOSPHERIC RIDGE RUNS 17ON IN ASSOCIATION WITH ANTICYCLONE
OVER MYANMAR, STEERING THE SYSTEM
WEST-NORTHWARDS, HOWEVER AS THE SYSTEM MOVES WEST-NORTHWARDS AND
ENTER SOUTHWEST BAY OF BENGAL AND IT
WILL LIE IN THE OUTER PERIPHERY OF THIS RIDGE, AND HENCE MOVE
NORTHWESTWARDS, AND CROSS SOUTH ANDHRA

PRADESH. AFTER THE LANDFALL IT WILL LIES CLOSE TO THE RIDGE AND HENCE
IT WILL MOVE INTO NORTHWARDS AND NORTH-
NORTHEAST WARDS. AT THE SIMULTANEOUSLY IT WILL INFLUENCE THE UPPER
TROPOSPHERIC TROUGH WHICH CURRENTLY RUNS

ALONG 65OE & IT WILL BE MOVING TOWARDS 75OE BY 3RD NOVEMBER 2026. IT
WILL ALSO NOT ALLOW THE SYSTEM TO
MOVE WESTWARDS RATHER IT WILL HELP IN RECURVING NORTH-NORTHEAST
WARDS.
THE TOTAL PRECIPITABLE WATER IMAGERY INDICATES WARM MOIST AIR
INCURSION INTO THE CORE FROM AROUND THE
SYSTEM AND ALSO SYSTEM FORECAST TRACK. HOWEVER, COLD AIR INCURSION IS
REACHING OUTER PERIPHERY OF THE
SYSTEM IN THE SOUTHWESTERN SECTOR FROM SOUTH INTERIOR PENINSULAR. AS
THE SYSTEM IS EXPECTED TO MOVE
TOWARDS SOUTH ANDHRA PRADESH, IT MAY NOT HELP IN WEAKENING THE
SYSTEM.
IR-WV IMAGERY INDICATES INTENSE CONVECTION (COLDER THAN -4

0C) TO THE NORTHEAST OF SYSTEM CENTRE. THUS

MJO, HIGH SST, LOW VERTICAL WIND SHEAR MAY SUPPORT FURTHER
DEVELOPMENT OF SYSTEM.
THE MODEL DIAGNOSIS BASED ON GLOBAL AND REGIONAL MODELS INDICATES,
THAT CURRENT HIGH LEVEL (LOW TO
MODERATE) WINDS SHEAR IS EXPECTED TO DECREASE BECOMING LOW WIND SHEAR
BY 00UTC OF 1ST NOVEMBER 2026.
THE LOW WIND SHEAR WILL CONTINUE TILL 00UTC OF 3RD NOVEMBER 2026
SUPPORTING INTENSIFICATION. MIDDLE LEVEL
RELATIVE HUMIDITY IS AT PRESENT ABOUT 70% WHILE IT IS EXPECTED TO
DECREASE SLIGHTLY BY 1ST NOVEMBER AND IT
MAY INCREASE THEREAFTER TILL 3RD NOVEMBER REACHING ABOUT 70-75%. THUS
SUPPORTS THE INTENSIFICATION.
ALL THE MODELS LIKE ECMWF, AI-FGN, AI-FCN, EC-AIFS, AURORA, GOOGLE
DEEPMIND AND HWRF ARE
INDICATING EVEN INTENSIFICATION OF CYCLONIC STORM/SEVERE CYCLONIC
STORM. GFS GROUP OF MODEL ARE SHOWING
AN INTENSITY OF LOW PRESSURE AREA ONLY. HOWEVER, THERE IS A VERY GOOD
CONSENSUS AMONG VARIOUS MODELS WRT
WEST-NORTHWESTWARDS MOVEMENT INITIALLY FOLLOWED BY NORTHWEST WARD
MOVEMENT TOWARDS SOUTH ANDHRA
PRADESH COAST. MANY OF AI MODELS AND ECMWF MODEL ARE SUGGESTING
NORTH-NORTHEAST WARDS OF RECURRING
AFTER LANDFALL, WHILE GFS SYSTEM SHOW WESTWARDS MOVEMENT INSIDE
SOUTHERN PENINSULAR AFTER LANDFALL.
HENCE CONSIDERING THE ENVIRONMENTAL FEATURES, CLIMATOLOGICAL GUIDANCE
AND MODEL GUIDANCE, MODERATE TO
HIGH PROBABILITY IS ASSIGNED FOR INTENSIFICATION INTO A SEVERE
CYCLONIC STORM BY 2ND NOVEMBER 2026.

CONFIDENCE LEVEL IN ESTIMATION OF:
(A) CURRENT LOCATION AND INTENSITY: HIGH
(B) FORECAST TRACK: HIGH
(C) FORECAST INTENSITY: MOD-HIGH=
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