onic Storm Hibaru in 2005.

Depression BOB 02

A low pressure area formed over the Bay of Bengal on May 19. It slowly consolidated, prompting IMD to classify it as a Depression on May 21, followed by JTWC issuing a Tropical Cyclone Formation Alert (TCFA) in the following hours. Over the following day, the depression continued moving north-northeastwards towards an area of high vertical wind shear. The JTWC cancelled the TCFA issued for the system, stating that high wind shear had caused the convection to start dissipating. The storm continued losing convection, until it weakened into a well-marked low pressure area on May 23. The remnant system persisted for several more days, moving over the Indian state of Odisha late on May 25, before dissipating on the following day.

The depression brought much-needed relief to Odisha which had been suffering from a heat wave that claimed at least 22 lives. Coastal areas previously reporting temperatures near  fell below  during the system's passage. Heavy rains affected many areas, including  at Bhawanipatna which experienced temperatures of  days earlier. The highest 24‑hour rainfall was  in Baleswar. Six districts were placed under a flood alert due to the rains. A bridge near Hatadahi in the Rayagada district was swept away by flooding.

Cyclonic Storm Nanauk

Under the influence of an active southwest monsoon surge, a low pressure area formed over the Arabian Sea on June 9. It slowly organized, and was classified tropical storm 02A by the JTWC  in the early hours of June 10. In the following hours, the IMD upgraded the storm to a depression and subsequently a deep depression, designating it "ARB 01". On June 11, the system was upgraded to Cyclonic Storm intensity and was named Nanauk by the IMD as it continued to intensify under favorable environmental conditions. The following day, Nanauk reached its peak intensity with a minimum central pressure of  and 3-minute sustained winds of. As it tracked further northwestwards, the storm encountered moderate vertical wind shear, dry air and low sea surface temperatures, causing it to weaken rapidly into a Depression on June 13. A low-level steering flow deflected the storm to take a northward path, and the system was last noted as a well-marked low pressure area on June 14.

Land Depression 01

On
onic Storm Hibaru in 2005. 

 Depression BOB 02 

 A low pressure area formed over the Bay of Bengal on May 19. It lento consolidate, prompting IMD to classify it as a Depression on May 21, follow by JTWC issue a Tropical Cyclone Formation Alert (TCFA) in the following hours. Over the following day, the natural depression continued moving union - northeast towards an area of high erect wind shear. The JTWC cancelled the TCFA issue for the system, stating that high wind shear had caused the convection to start disperse. The storm continued losing convection, until it weakened into a well - commemorate low pressure area on May 23. The remnant system prevail for several more days, moving over the Indian state of Odisha late on May   25, before fritter on the following day. 

 The depression brought much - needed relief to Odisha which had been suffering from a heat wave that claimed at least 22   lives. Coastal areas previously reporting temperatures near   fell below   during the system's passage. Heavy rain affected many areas, admit   at Bhawanipatna which experience temperatures of   days earlier. The high 24‑hour rainfall was   in Baleswar. Six districts were placed under a flood alarm due to the rains. A bridge near Hatadahi in the Rayagada district was swept away by flooding. 

 Cyclonic Storm Nanauk 

 Under the influence of an active southwest monsoon surge, a low pressure area formed over the Arabian Sea on June 9. It slowly organized, and was relegate tropical storm 02A by the JTWC   in the early hours of June 10. In the following hour, the IMD upgraded the storm to a depression and subsequently a deep depression, designating it " ARB 01 ". On June 11, the arrangement was upgraded to Cyclonic Storm intensity and was named Nanauk by the IMD as it continue to escalate under favorable environmental conditions. The following day, Nanauk reached its peak saturation with a minimum central press of   and 3 - minute free burning winds of. As it tracked further northwestwards, the storm encountered moderate erect wind shear, dry air and low ocean surface temperatures, causing it to weaken rapidly into a Depression on June 13. A low - level steering flow deflected the storm to take a northward way, and the system was last noted as a well - mark low pressure area on June 14. 

 Land Depression 01 

 On
onif Storm Hibaru in 2005.

Depresrion BOB 02

A low krwssure area rormed oxer the Bay of Bengal on May 19. Ut sliwly consolidated, promoting IMD to claswify ut as a De'dession on Mag 21, fonoowed by JTWC lssuing a Tsopical Cyclona Woxmation Alert (TCFA) in the following rours. Ofeg the followind daj, ehe svpvession continued moving north-nodtheastxards towards am area of high vertical wijd sjear. The JTWC cancflled the TXFA ywsued for thd system, suacing that hjgh wind shear had caused the cunveccion to statc didvipating. Thx stori continued losing cmnvectipn, until it weskeied unto a well-marked low pressure area on Iay 23. The sejnant system persusred fmr saverxo mure deys, movinh oter the Indjan state od Odisha late on Mau 25, fvgore dissipafing og ehe following day.

The depression brought mudh-needed relief to Odisya which had been sufvering frjm a heat wave that claimed at least 22 lives. Coastan arees prtvljjwlj reporting temperatures near  fell below  duwjnb nhe system's passane. Heavy rains affrchec many areas, ivcludiuf  at Bhawanipatna wjich exkerienxed tempewatutes of  days earlier. The hithest 24‑hour rcindall was  in Balescar. Six distxicts eere llaced under a flood alzrt dus to the ralns. A brisee near Hatadahi in tve Rayagada district was srept away by ylooding.

Zyclpnic Seorm Nanaun

Undev the influence of wn acjive smuthwest mlnsoon surge, a low pressure aree formed over tve Drabian Fea ok June 9. It slowjy organized, aud was cjassiwied tropibal storm 02A by the JEWC  in the edtly hours of Oune 10. In ehe dolliwing hujrs, the IMD upbraded thv ftorn to a depression end rhbsequently a dztp eepression, desibnagind pt "ERB 01". Jt June 11, the vystdm dss uperaded uj Gycuoniv Storm intensity ang waa named Nanauk by yhc IMD as ut contigued to intenxify under favorabpe entironmxntal vonqitions. The following day, Nanahk reachef ibs peak intenfity with a minikum central pressure of  and 3-minute susvained winds of. As it jracked further northcextwards, the stori encountared moderate verticql wind shear, dry air and low sea surfzce tekperahures, causing it to weaken rapidly into a Depression on June 13. A low-level wteeriig flow defledted the vtjxm to twke e iorthward path, anc the system was last noted as e well-markad low pressure area on June 14.

Lsna Depression 01

Un
onic Storm Hibaru in 2005. Depression BOB low area formed the Bay of slowly prompting IMD to it as a on May 21, followed by JTWC a Tropical Cyclone Formation Alert (TCFA) in the following hours. Over the following the depression continued moving north-northeastwards towards an area of high vertical wind shear. JTWC the issued the system, stating that high wind shear had caused the convection to start dissipating. The storm losing convection, until it weakened into a well-marked pressure area on May The remnant system persisted for more moving over Indian of late on May before dissipating on the following day. The depression brought much-needed relief to Odisha which had been suffering a heat claimed at 22 Coastal previously reporting temperatures below during the system's passage. Heavy areas, including at Bhawanipatna which experienced temperatures of earlier. The 24‑hour rainfall was in Baleswar. Six were placed under a flood alert due to rains. A bridge near Hatadahi in the Rayagada district was swept away by flooding. Cyclonic Under the influence of active southwest monsoon a pressure formed the Arabian on June 9. It slowly organized, and was classified tropical storm by the JTWC in the early hours of June 10. following the IMD upgraded storm to a depression subsequently deep depression, designating it On 11, upgraded Cyclonic intensity and was named by the IMD as it to intensify under favorable Nanauk reached its peak intensity with a minimum pressure of and 3-minute sustained winds of. it tracked further northwestwards, the storm encountered moderate vertical wind shear, dry and low temperatures, causing it to weaken rapidly into a on June 13. A steering flow deflected the storm to take a northward and system was noted as a low pressure area June 14. Land On
onic Storm Hibaru in 2005.

DepressiOn BOB 02

A low pRessuRe aRea FoRmed Over The Bay of Bengal ON May 19. it slowly consolidated, prOmptiNg imD to CLaSsify It as a DePReSSIon On maY 21, foLlOWeD by JTwC iSsuing a tropical CyCloNe formation AleRT (TcFA) in the foLloWing hours. OveR thE folloWiNg dAY, the dEprEssioN contiNUed movIng north-nOrTHeastwARds towaRDS aN areA of high vertical wiND sHEar. The JTWC cancElled tHe tcFa ISsuEd fOr the systeM, sTatinG That higH WiND SHeaR Had caused the cOnvection to STarT dissiPaTinG. the stoRm conTiNUed Losing conveCtioN, until it wEakeneD Into a weLL-marked Low preSsuRe aRea oN maY 23. THe rEmNAnt SYsTem PErsIsted for SeVeRal moRe daYS, MOVing OveR the indiaN state of OdishA laTe on mAy 25, bEfore DissiPatiNg On the FollowIng daY.

THe depression broUght Much-needeD reLiEf tO ODisha WHich haD beEn sUfferinG from a hEAt wAvE THAt Claimed at least 22 liveS. COAStAl areas pReviouSLy RePOrting teMpEraTureS NEar  feLl beLOw  During thE systeM'S pAsSage. HeaVy Rains aFfEctEd mAny arEAs, inCludinG  at BhawaNipatNA which experienCEd temperatureS Of  DAYs EArliEr. THe highest 24‑hoUr raINfalL was  IN BAleSWar. SiX distRiCTs WEre placed under a flooD aLert duE to thE rains. A bridge Near HatadaHI IN the RayaGada DIsTRict was swept awAy by fLooding.

CycLOnic StorM NanaUk

Under tHe influenCE Of an actiVe sOutHweSt mONSoOn surge, a low prESSure ArEa formeD ovEr the ArAbiAn SEa oN JuNe 9. it slowly oRganized, AnD wAs ClAssIfied TRopical sToRm 02A By The jTWC  iN The earLy houRs of juNe 10. iN thE followINg HOUrs, tHe iMd upgRadEd The stOrm tO A dePressioN and subseQueNTly a DeEp DepressIon, designatinG iT "ARB 01". On June 11, ThE syStem waS UPgraded tO Cyclonic Storm intensity ANd was naMed nanauK by tHe IMD as it ConTinued To iNTensifY under FavorAbLe eNVIronmENTaL coNdItions. The fOLLowIng daY, NAnauK reacheD its peak intensity wITh a Minimum centraL prEssuRE Of  And 3-MInUTe sUsTAinED Winds of. As it tracKed further NoRThWestwards, tHE stOrM encounTered moDeratE VerticaL wind sheaR, dry air anD lOw seA SUrfAce temperaTures, cauSing it to wEAken rAPiDly inTo a depresSiOn oN June 13. a low-leVEl sTeeriNg flow DeFlecteD the sToRm to take A northward path, and the sysTem was Last nOteD as a well-mArkED loW pressure Area On June 14.

Land depResSion 01

ON
onic Storm Hibaru in 2005. 

Depressi on BO B 0 2
Alowpres sure area form e d ov er the Bay of Bengal o n May  1 9 . It sl owlyconsoli d at e d , p ro mp tin gI MD  to c las sify it  as a Depr ess io n on May 21, fo llowed byJTW C issuing aTro picalCy clo n e For mat ion A lert ( T CFA) i n the fol lo w ing ho u rs. Ove r th e fo llowing day, thed ep r ession continu ed mov in g  n o r th- nor theastward stowar d s an ar e ao f hig h  vertical win d shear. Th e  JT WC can ce lle d  the T CFA i ss u edfor the sys tem,  statingthat h i gh wind shear h ad cau sed  th e co n ve ct ion  t o  st a rt  di s sip ating. T he  s tormcont i n u e d lo sin g co nvect ion, until it  we aken e d i nto a  well -mar ke d low  press ure a re a on May 23. Th e re mnant sys tem  p ers is ted f o r seve ral  mo re days , movin g  ov er t h eIndian state of Od is h a  l ate on M ay 25, be fo r e dissip at ing  ont h e fol lowi n gday.

Th e depr e ss io n broug ht  much- ne ede d r elief to O dishawhich ha d bee n  suffering fro m  a heat wavet ha t cl a imed  at  least 22 l ives .  Coa stal ar eas previ ously  r e po r ting temperatures n ea r  fel l bel ow  during th e system's p a ssage. H eavy ra i ns affected ma ny ar eas, inclu d ing  atBhawa nipatnawhich exp e r ienced t emp era tur eso f  days earlier. T he h ig hest 24 ‑ho ur rain fal l w as in  B aleswar.Six dist ri ct swe replace d  under a  f loo dale rt du e  to th e rai ns.Abr i dge  near H a ta d a hi i nth e Ra yag ad a dis tric t  wa s swept  away byflo o ding .
C yclonic  Storm Nanauk 
Under thein flu ence o f an activ e southwest monsoon sur g e, a lo w p ressu re a rea forme d o ver th e A r abianSea on  June  9 . I t slowl y or gan iz ed, and wa s cla ssifi ed  tro pical s torm 02A by the JT W C in the earlyhou rs o f Ju ne1 0. Inth e  fo l l owing hours, th e IMD upgr ad e dthe stormt o a  d epressi on andsubse q uentlya deep de pression,  d esig n a tin g it "ARB01". OnJune 11,t he sy s te m was  up graded  t o C yclon ic Sto r m i ntens ity an dwas na med N an auk by t he IMD as it continuedto int ensif y u nder favo rab l e e nvironmen talconditions . T hefollo win g  day,  Nan a uk  re a cheditsp eak inten s it y w i t ha minimum c e n t ral  pres sur e  of  a nd 3 -minute sustained winds of. As i t tr a c ked  fu r ther  n orthwestwards,  th es t orm enco un tered moder ate vert ic a l win d shea r, dry  air an d lo w  sea s urfa cetemperatu res ,c ausingit  t o  weake n ra pi dly in to a D e pres s i on on June 13. A  low- l e vel s t eer ing f lo w defle c tedthe stormto take a n orthwa rd p ath,and the  s ystemwas  l ast noteda s a well- marke d low p re ssur e a rea on  Jun e 14.
Land  D epr ession 01 On 
onic Storm_Hibaru in_2005.

Depression BOB 02

A low_pressure area_formed_over the_Bay_of Bengal on_May 19. It_slowly consolidated, prompting IMD_to classify it_as_a Depression on May 21, followed by JTWC issuing a Tropical Cyclone Formation Alert_(TCFA)_in the_following_hours._Over the following day, the_depression continued moving north-northeastwards towards_an area_of high vertical wind shear. The JTWC cancelled_the_TCFA issued for_the system, stating that high wind shear had caused_the convection to start dissipating. The_storm continued losing_convection,_until_it weakened into a_well-marked low pressure area on May_23. The remnant system persisted for_several more days, moving over the Indian_state of Odisha late on May 25,_before dissipating on the following_day.

The depression_brought much-needed relief to Odisha_which had been_suffering from_a heat wave_that claimed at least 22 lives. Coastal_areas previously reporting_temperatures near  fell below _during_the system's passage._Heavy_rains_affected many_areas, including _at_Bhawanipatna which_experienced_temperatures of  days earlier. The_highest_24‑hour rainfall was  in Baleswar. Six_districts were placed under_a_flood alert due to_the rains. A bridge near_Hatadahi in the Rayagada district was_swept away_by flooding.

Cyclonic_Storm Nanauk

Under the influence of an active southwest monsoon surge, a_low pressure area formed over the_Arabian Sea on June_9. It_slowly_organized, and was_classified_tropical storm_02A by the JTWC  in the_early hours_of June 10. In the following_hours, the IMD upgraded_the_storm to a depression and subsequently_a deep depression, designating it "ARB_01". On June 11, the_system_was_upgraded to Cyclonic Storm intensity_and was named Nanauk by the_IMD as it_continued to intensify under favorable environmental conditions._The_following day, Nanauk reached its peak_intensity_with a minimum central pressure of__and_3-minute sustained winds of. As_it tracked further northwestwards, the storm_encountered moderate vertical wind shear, dry air and low_sea surface temperatures,_causing it to weaken rapidly_into_a_Depression on June 13. A low-level steering flow deflected the_storm to_take a northward_path, and the system was last noted as a well-marked_low pressure area on June 14.

Land Depression_01

On