 several of which were covered bridges built more than 100 years prior to the storm. Flooding in Vermont was considered the worst since the flood of November 1927, with uninsured losses alone reaching about $733 million. The other states of New England experienced extensive flooding, but to a less degree. The storm left at least 58 deaths and about $15.8 billion in damage in the United States, which makes it the seventh costliest hurricane in the country. The remnants of Irene also brought flooding to Canada, especially Quebec. One death and about $130 million in insured damage were reported.

Tropical Depression Ten

A well-organized tropical wave moved into the eastern Atlantic on August 22. Tracking westward at a fast pace, the wave gradually developed shower and thunderstorm activity and a closed center of low pressure. Curved bands extended from the center by 00:00 UTC on August 25, indicating the development of a tropical depression; at this time, the system was centered about 405 mi (650 km) west-southwest of the southernmost Cape Verde Islands. Unfavorable northeasterly shear prevented intensification, with the depression peaking with winds of 35 mph (55 km/h) and a minimum pressure of 1006 mbar (hPa; 29.71 inHg) at the time of formation. As a mid-level ridge to the north of the cyclone weakened, it turned west-northwest while gradually weakening. By late on August 26, little convection existed over the center of circulation. At 00:00 UTC on August 27, the depression degenerated into a remnant area of low pressure and dissipated a few hours later after the center deteriorated into a trough.

Tropical Storm Jose

A mesoscale convective system developed north of an upper-level low east-southeast of Bermuda on August 25. A small mid-level area of low pressure formed on the western side of the convective complex later that same day, gradually developing into the lower levels of the atmosphere. As convection near the center of circulation increased in coverage and intensity, the system developed into a tropical depression at 06:00 UTC on August 26. Six hours later, the depression intensified into Tropical Storm Jose. After formation, strong wind shear from nearby Hurricane Irene slowed, and eventually halted, development trends. Jose attained its peak intensity with winds of 45 mph (75 km/
several of which were covered bridges built more than 100   days prior to the storm. implosion therapy in Vermont was considered the worst since the flood tide of November 1927, with uninsured losses entirely reaching about $ 733   million. The other state of New England feel extensive implosion therapy, but to a less academic degree. The storm left at least 58   deaths and approximately $ 15.8   billion in damage in the United States, which makes it the seventh costly hurricane in the area. The remnants of Irene also brought flooding to Canada, especially Quebec. One end and about $ 130   million in insured damage were report. 

 Tropical Depression Ten 

 A well - organized tropical wave moved into the easterly Atlantic on August   22. Tracking westward at a debauched pace, the wave gradually developed shower and thunderstorm activity and a closed plaza of low pressure. Curved bands extended from the center by 00:00   UTC on August   25, indicating the development of a tropical depression; at this time, the system was centered about 405   mi (650   km) west - southwest of the southernmost Cape Verde Islands. Unfavorable northeasterly shear prevented intensification, with the depression peaking with winds of 35   mph (55   km / h) and a minimal press of 1006   mbar (hPa; 29.71   inHg) at the time of geological formation. As a mid - degree ridge to the north of the cyclone weakened, it turned west - northwest while gradually weaken. By belated on August   26, little convection existed over the plaza of circulation. At 00:00   UTC on August 27, the depression degenerated into a remnant area of low pressure and dissipated a few hour later after the center deteriorated into a trough. 

 Tropical Storm Jose 

 A mesoscale convective arrangement developed north of an upper - floor low east - southeast of Bermuda on August   25. A small mid - level area of low atmospheric pressure formed on the western side of the convective building complex later that like day, gradually developing into the lower levels of the atmosphere. As convection near the kernel of circulation increased in coverage and intensity, the arrangement developed into a tropical natural depression at 06:00   UTC on August   26. Six hours subsequently, the depression intensify into Tropical Storm Jose. After formation, strong wind shear from nearby Hurricane Irene slowed, and eventually stem, development trends. Jose attained its peak intensity with winds of 45   mph (75   km/
 segeral of which were coveved bridges builj nore tian 100 yeads prior to the storm. Flooding in Vecmonr was considered the worst rince the flood od Notember 1927, with uniiaured losses zpone ceaching about $733 killion. Tha other states ow Uew England experienced extensive fljoding, nuh to a less dedree. Ehe anovm left at least 58 deaths and abouf $15.8 billimn in damage on the United States, which makfs it the seventh fostliest hodrisqne in the cuuntry. The remnants of Irene also brought flooding to Canaba, especialoy Quftec. One deavh and about $130 million in invured dsmage were repprtxd.

Tripical Depression Ten

E well-organized tropycal wave mkved into the easreen Atnanthc ov Aueusu 22. Tcaciing wfstxard at a fzst pace, thw wave gradually defejiped shower ahd thugdqrstorm activity and a closed center of los pressure. Curved bands extended from the cejter by 00:00 UEC on August 25, indicating the development of a trophcal veorewslon; xr hhis time, the system was centered about 405 mi (650 km) sext-xouthwest of tme southernmost Cale Vrtde Islands. Unwavorayme northeasterly shewr prevgnted untensifisatipn, with the depression peakung with winbs if 35 mph (55 km/h) and a mnnimum pressbre of 1006 mbar (hPa; 29.71 inHg) at the time oy formztion. As a lid-level dkdge to the nortf on tve cyclone weakened, it turged west-nirthcest whiue gtaduallr weakeninh. By late on August 26, littpe couvecthon existef over the center of circulatioi. At 00:00 UTC on Aoguvt 27, the depxessiok degenerated igto a remnant crea of jow pfessure ans dissi'ated a few rours later axjer the centec deteriowatee inro a trujgh.

Tropical Stprm Jose

A mesoscale convective system dexsloped north of an upper-level low eart-sjunheest os Bermuda on Dugurt 25. X smalu mid-level crda og low pressure formeg on the western side pf the concective somplex later that same day, grafuallb deveuopinb igto the lower levels of the atjosphere. Ws gonvection newr tme cgnter of cixculation increased in coverage and inteisity, the system developed into a tropical cepression et 06:00 UTC on Augusd 26. Six hours later, thw depression inteksified into Tropical Atorm Bose. Wfter formation, strong wind shear from nearby Hurricane Irene slowed, and wventueljy halted, dsvelppmenn txenbs. Jose atteiied its peak intemsity with winds of 45 mph (75 km/
several of which were covered bridges built 100 prior to storm. Flooding in since flood of November with uninsured losses reaching about $733 million. The other of New England experienced extensive flooding, but to a less degree. The storm at least 58 deaths and about $15.8 billion in damage in the United which it seventh hurricane in the country. The remnants of Irene also brought flooding to Canada, especially Quebec. One and about $130 million in insured damage were Tropical Depression Ten A tropical wave moved into the Atlantic August 22. westward a pace, the wave developed shower and thunderstorm activity and a closed center of low pressure. Curved bands extended from the by 00:00 August 25, the of tropical depression; at the system was centered about 405 west-southwest of the southernmost Cape Verde Islands. Unfavorable shear prevented with the depression peaking with winds 35 mph (55 km/h) and a minimum pressure 1006 mbar (hPa; 29.71 inHg) at the time of formation. As a mid-level ridge to of the cyclone weakened, turned west-northwest while weakening. late August little convection over the center of circulation. At 00:00 UTC on August 27, depression degenerated into a remnant area of low pressure and few later after the deteriorated into a trough. Storm A mesoscale convective system of upper-level Bermuda August A small mid-level area low pressure formed on the side of the convective gradually developing into the lower levels of the As convection near the center of circulation in coverage and intensity, the system developed into a tropical depression at UTC on Six hours later, the depression intensified into Tropical Jose. After formation, strong shear from nearby Hurricane Irene slowed, and eventually halted, trends. attained its intensity with winds 45 mph (75
 several of which were covered Bridges buiLt morE thAn 100 yEaRs prIor tO the storm. FloodINg in vermont was considered thE worsT sINce tHE fLood oF NovembER 1927, wITH unInSuRed LoSSeS alonE reAching aBout $733 millioN. ThE oTher states of nEw england expEriEnced extensiVe fLoodinG, bUt tO A less DegRee. ThE storm LEft at lEast 58 deathS aND about $15.8 BIllion iN DAmAge iN the United States, wHIcH Makes it the seveNth cosTlIEsT HUrrIcaNe in the couNtRy. The REmnants OF IRENE alSO brought floodIng to Canada, ESpeCially quEbeC. one deaTh and AbOUt $130 mIllion in insUred Damage werE reporTEd.

TropiCAl DepreSsion TEn

A WelL-orgANiZeD trOpICal WAvE moVEd iNto the eaStErN AtlaNtic ON aUGust 22. traCkinG westWard at a fast paCe, tHe waVE grAdualLy devElopEd ShoweR and thUnderStOrm activity and a ClosEd center oF loW pResSuRe. CurVEd bandS exTenDed from The centER by 00:00 uTc ON auGust 25, indicating the dEvELOpMent of a tRopicaL DePrESsion; at tHiS tiMe, thE SYstem Was cENtEred abouT 405 mi (650 km) wESt-SoUthwest Of The souThErnMosT Cape vErde islandS. UnfavorAble nORtheasterly sheAR prevented intENsIFIcATion, WitH the depressIon pEAkinG witH WiNds OF 35 mph (55 kM/h) and A mINiMUm pressure of 1006 mbar (hPa; 29.71 Inhg) at thE time Of formation. As A mid-level rIDGE to the noRth oF ThE Cyclone weakeneD, it tuRned west-noRThwest whIle grAdually wEakening. BY LAte on AugUst 26, LitTle ConVECtIon existed oveR THe ceNtEr of cirCulAtion. At 00:00 uTC On AUguSt 27, tHe DepressioN degenerAtEd InTo A reMnant ARea of low PrEssUrE anD dissIPated a Few hoUrs lAtEr AFteR the cenTEr DETeriOrAtEd inTo a TrOugh.

TRopiCAl STorm JosE

A mesoscaLe cONvecTiVe System dEveloped north Of An upper-levEl Low East-soUTHeast of BErmuda on August 25. A small mid-LEvel areA of Low prEssuRe formed oN thE westeRn sIDe of thE conveCtive CoMplEX Later THAt SamE dAy, graduallY DEveLopinG iNto tHe lower Levels of the atmosphERe. AS convection neAr tHe ceNTEr Of cIRcULatIoN IncREAsed in coverage aNd intensitY, tHE sYstem develOPed InTo a tropIcal depRessiON at 06:00 UTC oN August 26. SiX hours latEr, The dEPResSion intensIfied intO Tropical sTorm JOSe. after ForMation, StRonG wind Shear fROm nEarby hurricAnE Irene SloweD, aNd eventuAlly halted, development trEnds. JoSe attAinEd its peak IntENsiTy with winDs of 45 Mph (75 km/
 several of which were cov ered bridg es bu ilt  mo re  tha n 10 0 years priort o th e storm. Flooding in V ermon tw as c o ns idere d the w o rs t sin ce  t hefl o od  of N ove mber 19 27, with u nin su red losses a l on e reaching  ab out $733 mil lio n. The  o the r  stat esof Ne w Engl a nd exp eriencedex t ensive floodin g ,  b ut t o a less degree.T he storm left atleast58 de a t hsand  about $15 .8  bill i on in d a ma g e int he United Sta tes, whichm ake s it t he  se v enth c ostli es t  hu rricane inthecountry.The re m nants o f  Irenealso b rou ght  flo o di ng  to  C a nad a ,esp e cia lly Queb ec .One d eath a n d  abo ut$130  mill ion in insure d d amag e  we re re porte d.
Tr opica l Depr essio nTen

A well-org aniz ed tropic alwa vemo ved i n to the  ea ste rn Atla ntic on Aug us t 2 2.  Tracking westward  a t afast pac e, the wa ve graduall ydev elop e d  show er a n dthunders torm a c ti vi ty andaclosed  c ent erof lo w  pre ssure.  Curvedbands extended fromt he center by0 0: 0 0  U T C on  Au gust 25, in dica t ingthed ev elo p mentof atr o pi c al depression; at t hi s time , the  system was c entered ab o u t  405 mi(650 km )  west-southwes t ofthe southe r nmost Ca pe Ve rde Isla nds. Unfa v o rable no rth eas ter lys h ea r prevented i n t ensi fi cation,  wi th thedep res sio n p ea king with  winds o f35  m ph  (5 5 km/ h ) and ami nim um  pr essur e  of 10 06 mb ar ( hP a; 29. 71 inHg )  a t theti me  offor ma tion.  Asa  mi d-level  ridge to  th e  nor th  o f the c yclone weaken ed , it turne dwes t-nort h w est whil e gradually weakening.B y lateonAugus t 26 , littlecon vectio n e x istedover t he ce nt ero f  circ u l at ion .At 00:00 U T C  on  Augu st  27,  the de pression degenerat e d i nto a remnant  ar ea o f lo w p r es s ure  a n d d i s sipated a few h ours later  a f te r the cent e r d et eriorat ed into  a tr o ugh.

T ropical S torm Jose 
A me s o sca le convect ive syst em develo p ed no r th  of a n u pper-l ev ellow e ast-so u the ast o f Berm ud a on A ugust  2 5. A sma ll mid-level area of lo w pres surefor med on th e w e ste rn side o f th e convecti vecom plexlat e r tha t sa m eday ,  grad uall y  developi n gint o th e lower lev e l s  of  theatm o sphere . As  convection neart he center of c ircu l a tio n i n crea se d in coverageand  i n t ensity,th e system de velopedin t o a t ropica l depr essiona t  0 6 :00 UT C on  Au gust 26.Six  h o urs lat er ,t he dep ress io n inte nsifie d  int o Tropical Storm J ose.A f ter f o rma tion,  s trong w i nd s hear fromnearby Hurr icaneIren e slo wed, an deventu all yhalted, de v elopmenttrend s. Jose  a ttai ned  its p eaki n tensi ty w it h w inds of 4 5 mp h  ( 75 km/ 
 several_of which_were covered bridges built_more than_100 years_prior to_the_storm. Flooding in_Vermont was considered_the worst since the_flood of November_1927,_with uninsured losses alone reaching about $733 million. The other states of New England experienced_extensive_flooding, but_to_a_less degree. The storm left_at least 58 deaths and about_$15.8 billion in_damage in the United States, which makes it_the_seventh costliest hurricane_in the country. The remnants of Irene also brought_flooding to Canada, especially Quebec. One_death and about_$130 million_in_insured damage were reported.

Tropical_Depression Ten

A well-organized tropical wave moved_into the eastern Atlantic on August 22._Tracking westward at a fast pace, the_wave gradually developed shower and thunderstorm_activity and a closed center_of low_pressure. Curved bands extended from_the center by_00:00 UTC on_August 25, indicating the_development of a tropical depression; at_this time, the_system was centered about 405 mi (650 km)_west-southwest_of the southernmost_Cape_Verde_Islands. Unfavorable_northeasterly shear prevented_intensification,_with the_depression_peaking with winds of 35 mph (55 km/h)_and_a minimum pressure of 1006 mbar (hPa; 29.71 inHg)_at the time of_formation._As a mid-level ridge_to the north of the_cyclone weakened, it turned west-northwest while_gradually weakening._By late_on August 26, little convection existed over the center of circulation. At_00:00 UTC on August 27, the depression_degenerated into a remnant_area of_low_pressure and dissipated_a_few hours_later after the center deteriorated into a_trough.

Tropical Storm_Jose

A mesoscale convective system developed north_of an upper-level low_east-southeast_of Bermuda on August 25. A small_mid-level area of low pressure formed_on the western side of_the_convective_complex later that same day,_gradually developing into the lower levels_of the atmosphere._As convection near the center of circulation_increased_in coverage and intensity, the system_developed_into a tropical depression at 06:00 UTC_on_August 26._Six hours later, the depression_intensified into Tropical Storm Jose. After_formation, strong wind shear from nearby Hurricane Irene slowed,_and eventually halted,_development trends. Jose attained its_peak_intensity_with winds of 45 mph (75 km/