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91.28645324707031 43 WikiText2
5750 When the need for a light armoured vehicle became apparent to the Israeli security forces , AIL 's engineering department designed a vehicle protection system from the bottom up , integrating it into the existing vehicle in a manner that did not compromise its off @-@ road and other capabilities , and that did not create the mechanical strain and increase in maintenance often associated with up @-@ armouring , in part due to its computerized 180 horsepower ( 130 kW ) injected engine .
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5751 The armour protects against 7 @.@ 62 × 39mm ( 0 @.@ 3 in ) armour @-@ piercing ammunition , and maintains a high protection @-@ to @-@ weight and cost ratio by employing IDF approved advanced materials . The protected Israeli configuration 's gross vehicle weight is 3 @,@ 000 kilograms ( 6 @,@ 614 lb ) , though several varying protection levels are in use with individual units .
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5752 Another important asset are the Storm 's narrow dimensions , which allow it to traverse the narrow alleyways common to the casbahs of many Middle Eastern cities , places that armoured Humvees can only enter with great difficulty and minimal manoeuvrability , if at all . Full @-@ height rear doors which allow for the quick deployment of fully equipped troops into combat are touted as another advantage over similar vehicles .
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5753 = = = Civilian use = = =
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5754 First generation Storms were made available to the general public in Israel from 1992 to 2001 . A small number were purchased directly by private consumers , while larger numbers were acquired second @-@ hand from Israeli government @-@ owned firms like the Israel Electric Company and Mekorot water company , as well as National Parks Authority and Israel Police . Modified Storms are popular with off @-@ roading enthusiasts in Israel .
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5755 = = Storm II = =
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5756 Beginning in 2006 , AIL began delivery of an improved model to the IDF , the M @-@ 242 Storm Mark II , known in the field as the " Storm Commander " . A number of significant changes have been incorporated into the new TJ @-@ based Storms stemming from soldiers ' feedback , updated operational requirements , and testing by GOC Army Headquarters and Logistics , Medical , and the Centers Directorate . Perhaps the most obvious change is the addition of dual passenger doors , making the Storm II the first five @-@ door Jeep Wrangler derivative .
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5757 Other improvements include the change to a manual transmission with six forward speeds ( instead of the previous four ) , and increased stability resulting from wider track axles than its predecessor . Leaf springs were replaced with modern coil spring suspension front and rear , and the Storm II features rear Dana 44 axles and front TJ Dana 30s , factory designed slip yoke eliminators , and the added safety of standard airbags . Soldiers ' comfort was addressed as well with the addition of standard rear air conditioning and a compact disc player .
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5758 Storm II is also produced in an armoured version , and is offered with an optional 2 @.@ 8 litre VM Motori turbodiesel , automatic transmission , right hand drive , and run @-@ flat tyres . AIL is capable of completing ten vehicles daily . Due to recently passed tax laws , a civilian version is not yet available in the local market .
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5759 = = = MDT David controversy = = =
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5760 Developed in the 2000s at an investment of US $ 2 million after IDF commitments for 1 @,@ 200 units , some AIL jobs were believed to be in jeopardy following a mid @-@ 2005 announcement that the IDF would purchase 100 US sold Land Rover Defender @-@ based MDT David . The announcement provoked threats of protests from AIL 's management and labourers , who had recently faced the blow of local Humvee assembly ceasing due to budget considerations . The MDT David was chosen over the armoured version of the Storm because the heavy Storm was said to suffer from handling and reliability problems , safety hazards and limited mission operability . However the IDF said that the purchase of the David was to fill a temporary gap in production until the Storm II 's testing was completed , and has since begun filling its commitment .
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5761 = = Storm III = =
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5762 A Storm Mark III was set to be produced for the Israeli defense forces starting in June 2008 , when the IDF was to purchase around 600 vehicles beginning in early 2011 . Based on the then new four @-@ door Jeep Wrangler JK design , the Mark III is meant to address some of the shortfalls of the earlier Mark II . Whereas the previous vehicle was an update of the original TK Storm , the Storm III was designed from the outset with a five @-@ door configuration . Unlike the TJ @-@ L , the new JK Storm has a much higher maximum load capacity in part due to heavier @-@ duty shock absorbers , springs and axles , necessary for an armored version . It includes a standard 2.8L VM Motori turbodiesel and automatic transmission .
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5763 Like the Storm II , the Mark III was initially available only to the military with versions set to be delivered to the Israel Police in 2009 . A civilian version would only be released if the local tax code was modified to allow it to compete with foreign imports of the same class . AIL states that if such a thing would happen , a petrol engine version could be offered . Regarding Export markets , the Storm 3 has already seen use in several countries , especially in its armored version .
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5764 A pair of production J8 's was tested by Israeli web magazine Jeepolog.com journalists in April 2009 . It was dubbed " probably , the best Jeep ever " .
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5765 = = = Commander version = = =
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5766 The commander version incorporates a 5 @-@ door hard top cab allowing for the quick and convenient entrance and exit of the driver and all passengers or troops . A large rear compartment enables the storage of both cargo and communications equipment .
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5767 This version comes equipped with an air conditioning system providing maximum comfort in hot climatic conditions . A roll over protection structure ( ROPS ) maximizes safety conditions for passengers .
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5768 = = = Armored version = = =
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5769 The armored version of the Storm 3 , designed for protection against light weapon threats , incorporates a heavy duty transfer case and a specially designed suspension system which includes heavy duty springs ( front - coil , rear - leaf ) and shock absorbers , together with rigid heavy duty axles allowing for a smooth and safe ride on both rough terrain as well as regular highways .
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5770 = = = Reconnaissance & Patrol version = = =
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5771 The Storm 3 reconnaissance and patrol model allows for extra stowage of fuel , water and equipment . This version is especially suited to be fitted with various machine gun or special equipment mountings .
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5772 = 1940 Atlantic hurricane season =
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5773 The 1940 Atlantic hurricane season was a generally average period of tropical cyclogenesis in 1940 . Though the season had no official bounds , most tropical cyclone activity occurred during August and September . Throughout the year , fourteen tropical cyclones formed , of which nine reached tropical storm intensity ; six were hurricanes . None of the hurricanes reached major hurricane intensity . Tropical cyclones that did not approach populated areas or shipping lanes , especially if they were relatively weak and of short duration , may have remained undetected . Because technologies such as satellite monitoring were not available until the 1960s , historical data on tropical cyclones from this period are often not reliable . As a result of a reanalysis project which analyzed the season in 2012 , an additional hurricane was added to HURDAT . The year 's first tropical storm formed on May 19 off the northern coast of Hispaniola . At the time , this was a rare occurrence , as only four other tropical disturbances were known to have formed prior during this period ; since then , reanalysis of previous seasons has concluded that there were more than four tropical cyclones in May before 1940 . The season 's final system was a tropical disturbance situated in the Greater Antilles , which dissipated on November 8 .
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5774 All three hurricanes in August brought flooding rainfall to areas of the United States . The first became the wettest tropical cyclone recorded in Louisiana history . The second hurricane impacted regions of the Southeastern United States , producing record precipitation and killing at least 52 people . Despite not making landfall , the third hurricane in August interacted with a stationary front over the Mid @-@ Atlantic states , resulting in localized flooding and thus making the tropical cyclone the wettest in New Jersey history . This hurricane would also be the strongest in the hurricane season , with maximum sustained winds of 110 mph ( 175 km / h ) and a minimum barometric pressure of 961 mbar ( hPa ; 28 @.@ 39 inHg ) , making it a high @-@ end Category 2 hurricane on the modern @-@ day Saffir – Simpson hurricane wind scale . Activity decreased in September , though a damaging hurricane swept through areas of the Canadian Maritimes , resulting in large crop and infrastructural losses . Two tropical cyclones of at least tropical storm strength were recorded in October , though neither resulted in fatalities . Collectively , storms in the hurricane season caused 71 fatalities and $ 29 @.@ 329 million in damages . The 1940 South Carolina hurricane , which swept through areas of the Southeastern United States in August , was the most damaging and deadly of the tropical cyclones .
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5775 = = Storms = =
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5776 = = = Tropical Storm One = = =
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5777 On May 18 , a weak low @-@ pressure area was detected south of Hispaniola . Moving northward , the low became sufficiently organized to be classified as a tropical storm at 1200 UTC on May 19 , southeast of Turks Island . At the time , ship observations indicated that the disturbance had a well @-@ defined cyclonic circulation , with the strongest winds situated in the northern semicircle of the cyclone . Continuing northward , the tropical storm gradually intensified and attained maximum sustained winds of 65 mph ( 100 km / h ) by 0000 UTC on May 22 . The Belgian ship M.S. Lubrafol recorded a peripheral barometric pressure of 996 mbar ( hPa ; 29 @.@ 42 inHg ) ; this was the lowest pressure measured in connection with the storm . The following day , the tropical storm temporarily curved towards the east @-@ southeast before recurving back towards a northeast direction . At the same time , the storm expanded in size and began to transition into an extratropical cyclone . By 1200 UTC , the cyclone completed its extratropical transition , due to the entrainment of colder air . The remnant system persisted until 0600 UTC on May 27 .
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5778 = = = Hurricane Two = = =
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5779 On August 3 , an extratropical cyclone developed into a tropical depression off the west coast of Florida . Initially a weak disturbance , it moved generally westward , slowly gaining in intensity . Early on August 4 , the depression attained tropical storm intensity . Ships in the vicinity of the storm reported a much stronger tropical cyclone than initially suggested . After reaching hurricane strength on August 5 south of the Mississippi River Delta , the storm strengthened further into a modern @-@ day Category 2 hurricane , with maximum sustained winds of 100 mph and a minimum barometric pressure of 972 mbar ( hPa ; 28 @.@ 71 inHg ) at 0600 UTC on August 7 . The hurricane moved ashore near Sabine Pass , Texas later that day at peak strength . Once inland , the storm executed a sharp curve to the north and quickly weakened , degenerating into a tropical storm on August 8 before dissipating over Arkansas on August 10 .
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5780 Reports of a potentially destructive hurricane near the United States Gulf Coast forced thousands of residents in low @-@ lying areas to evacuate prior to the storm moving inland . Offshore , the hurricane generated rough seas and a strong storm surge , peaking at 6 @.@ 4 ft ( 1 @.@ 95 m ) on the western edge of Lake Pontchartrain . The anomalously high tides flooded many of Louisiana 's outlying islands , inundating resorts . Strong winds caused moderate infrastructural damage , primarily in Texas , though its impact was mainly to communication networks along the U.S. Gulf Coast which were disrupted by the winds . However , much of the property and crop damage wrought by the hurricane was due to the torrential rainfall it produced in low @-@ lying areas , setting off record floods . Rainfall peaked at 37 @.@ 5 in ( 953 mm ) in Miller Island off Louisiana , making it the wettest tropical cyclone in state history . Nineteen official weather stations in both Texas and Louisiana observed record 24 @-@ hour rainfall totals for the month of August as a result of the slow @-@ moving hurricane . Property , livestock , and crops – especially cotton , corn , and pecan crops – were heavily damaged . Entire ecosystems were also altered by the rainfall . Overall , the storm caused $ 10 @.@ 75 million in damages and seven fatalities .
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5781 = = = Hurricane Three = = =
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5782 A storm of potentially Cape Verde origin was detected in the Virgin Islands at 1800 UTC on August 5 . Initially moving westward , the tropical storm gradually gained in intensity before making a sharp curve towards the north on August 8 . The storm continued in a northerly motion before a second curvature brought it in a generally westward direction on August 9 . Shortly after , the tropical storm reached hurricane intensity as a modern @-@ day Category 1 hurricane . The hurricane eventually made landfall at peak intensity on Hilton Head Island , South Carolina at 2030 UTC on September 21 . At the time , the storm had maximum sustained winds of 100 mph ( 155 km / h ) and a minimum central pressure of 972 mbar ( hPa ; 28 @.@ 71 inHg ) , equivalent to a modern @-@ day Category 2 hurricane . Once inland , the tropical cyclone gradually weakened , and recurved northeastward before dissipating over the Appalachian Mountains on August 14 .
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5783 The hurricane dropped torrential rainfall over the Southeast United States , causing unprecedented devastation in the region . The storm was considered the worst to impact in the region in at least 29 years . Precipitation peaked at 20 @.@ 65 in ( 525 mm ) in Idlewild , North Carolina . The heavy rainfall caused streams to greatly exceed their respective flood stages , damaging waterfront property . Many of the deaths occurred in North Carolina , where 30 people died . Transportation was disrupted as a result of the debris scattered by the wind and rain . In Caldwell County alone , 90 percent of bridges were swept away . Overall , the storm caused 50 fatalities and $ 13 million in damages .
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5784 = = = Hurricane Four = = =
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5785 On August 26 , a low @-@ pressure area in the open Atlantic Ocean became sufficiently organized to be classified as a tropical cyclone . Moving slowly in a general west @-@ northwest motion , the disturbance intensified , reaching tropical storm strength on August 28 and subsequently hurricane intensity on August 30 . The hurricane passed within 85 mi ( 135 km ) of Cape Hatteras before recurving towards the northeast . However , the hurricane continued to intensify , and reached peak intensity as a modern @-@ day Category 2 hurricane with maximum sustained winds of 110 mph ( 175 km / h ) and a minimum barometric pressure of 961 mbar ( hPa ; 28 @.@ 38 inHg ) , though these statistical peaks were achieved at different times on September 2 . Afterwards , the tropical cyclone began a weakening trend as it proceeded northward , and had degenerated into a tropical storm by the time it made its first landfall on Nova Scotia later that day . The storm transitioned into an extratropical cyclone the next day while making another landfall on New Brunswick . The extratropical remnants persisted into Quebec before merging with a larger extratropical system late on September 3 .
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5786 Despite not making landfall on the United States , the hurricane caused widespread damage . Extensive precautionary measures were undertaken across the coast , particularly in New England . The heightened precautions were due in part to fears that effects from the storm would be similar to that of a devastating hurricane which struck the region two years prior . Most of the damage associated with the hurricane occurred in New Jersey , where the combination of moisture from the hurricane and a stationary front produced record rainfall , peaking at 24 in ( 610 mm ) in the town of Ewan . This would make the storm the wettest in state history . The resultant floods damaged infrastructure , mostly to road networks . Damage in the state amounted to $ 4 million . Further north in New England , strong winds were reported , though damage remained minimal . Although the storm made two landfalls in Atlantic Canada , damage too was minimal , and was limited to several boating incidents caused by strong waves . Overall , the hurricane caused $ 4 @.@ 05 million in damage , primarily due to flooding in New Jersey , and seven fatalities .
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5787 = = = Hurricane Five = = =
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5788 A tropical depression was first detected east of the Lesser Antilles on September 7 , though at the time weather observations in the area were sparse . The disturbance gradually intensified throughout much of its early formative stages , attaining tropical storm strength on September 10 ; further strengthening into a hurricane north of Puerto Rico occurred two days later . Shortly thereafter , the hurricane recurved northward , and reached peak intensity the following day as a modern @-@ day Category 2 hurricane with maximum sustained winds of 100 mph ( 160 km / h ) and a minimum barometric pressure of at least 988 mbar ( hPa ; 29 @.@ 18 inHg ) . The cyclone steadily weakened thereafter before making landfall on Nova Scotia on September 17 with winds of 85 mph ( 135 km / h ) . Moving into the Gulf of Saint Lawrence later that day , the storm transitioned into an extratropical cyclone . The remnant system curved eastward and passed over Newfoundland before dissipating over the Atlantic on September 19 .
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5789 While off of the United States East Coast , the hurricane caused numerous shipping incidents , most notably the stranding of the Swedish freighter Laponia off of Cape Hatteras , North Carolina on September 16 . Two other boat incidents resulted in two deaths . The hurricane also brought strong winds of tropical storm @-@ force and snow over areas of New England . In Atlantic Canada , a strong storm surge peaking at 4 ft ( 1 @.@ 3 m ) above average sunk or damaged several ships and inundated cities . In New Brunswick , the waves hurt the lobster fishing industry . In Nova Scotia , strong winds disrupted telecommunication and power services . The winds also severely damaged crops . Roughly half of apple production in Annapolis Valley was lost during the storm , resulting in around $ 1 @.@ 49 million in economic losses . Strong winds in New Brunswick caused moderate to severe infrastructural damage , and additional damages to crops occurred there . Overall , the hurricane caused three fatalities , with two off of the United States and one in New Brunswick .
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5790 = = = Tropical Storm Six = = =
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5791 A westward moving tropical depression developed in the southwestern Caribbean Sea just west of Bluefields , Nicaragua at 1200 UTC on September 18 . The following day , the depression intensified into a tropical storm at 0600 UTC . The tropical storm made landfall on the Mosquito Coast of Nicaragua at 1400 UTC , with winds of 40 mph ( 65 km / h ) . The cyclone weakened to a tropical depression over land , but reintensified back to tropical storm strength upon entry into the Gulf of Honduras on September 20 . The cyclone 's northwest motion caused it to make a second landfall near the border of Mexico and British Honduras at 0300 UTC on September 21 as a slightly stronger system with winds of 50 mph ( 85 km / h ) ; this would be the storm 's peak intensity . Over the Yucatán Peninsula , the tropical storm re @-@ weakened , but later intensified once again once it reached the Gulf of Mexico . In the Gulf , the storm made a gradual curve northward , before making a final landfall near Lafayette , Louisiana at 0900 UTC on September 24 with winds of 45 mph ( 75 km / h ) and a minimum barometric pressure of 1002 mbar ( hPa ; 29 @.@ 59 inHg ) . Once inland , the tropical cyclone curved eastward and weakened before dissipating the next day , after becoming absorbed by a frontal boundary .
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5792 Upon making landfall , the tropical storm produced strong winds over a wide area . The strongest winds were reported by a station in San Antonio , Texas , which reported 40 mph ( 65 km / h ) winds , far removed from the storm 's center ; these strong winds were likely due to squalls . Heavy rainfall was also reported , though the rains mainly occurred to the east of the passing tropical cyclone . Precipitation peaked at 10 in ( 254 mm ) in Ville Platte , Louisiana . The tropical storm produced three tornadoes over the Southern United States which collecitvely caused $ 39 @,@ 000 in damage and caused two fatalities . Two of the tornadoes formed in Mississippi while one formed in Louisiana . Several other people were also injured by the tornadoes .
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5793 = = = Hurricane Seven = = =
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5794 In late September , a tropical wave persisted in the northeastern Atlantic Ocean . The low @-@ pressure area later became sufficiently organized to be classified as a tropical storm at 0000 UTC on September 22 . The disturbance quickly organized after tropical cyclogenesis , and reached a strength equivalent to a modern @-@ day Category 1 hurricane strength at 1800 UTC later that day . The American steamship Otho encountered the system that day , and reported gale force winds in conjunction with a peripheral barometric pressure of 996 mbar ( hPa ; 29 @.@ 42 inHg ) . The tropical cyclone continued to the east @-@ northeast , where it gradually intensified . At 1200 UTC on September 23 , the hurricane attained modern @-@ day Category 2 hurricane intensity with winds of 100 mbar ( 155 km / h ) ; a peak which would be maintained for at least the following 12 hours . A second steamship , the Lobito , reported hurricane @-@ force winds along with a minimum pressure of 977 mbar ( hPa ; 28 @.@ 85 inHg ) ; this would be the lowest pressure measured associated with the tropical cyclone . After reaching peak intensity , the hurricane began a weakening trend , and degenerated to a Category 1 hurricane at 0600 UTC as it passed over the Azores . The following day , the hurricane recurved westward , where it weakened before transitioning into an extratropical cyclone on September 28 . This remnant system subsequently dissipated .
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5795 As the hurricane passed over the Azores , several weather stations reported low barometric pressures , with the lowest being a measurement of 984 mbar ( hPa ; 29 @.@ 06 inHg ) on Terceira Island at 0600 UTC on September 25 . As a result of the impending storm , several Pan Am Clipper flights to the archipelago were suspended for three consecutive days . The maximum reported gust in the Azores was an observation of 65 mph ( 100 km / h ) on September 25 . As a result of moving slowly over the islands , torrential rainfall was also reported . At Angra do Heroísmo , 13 @.@ 11 in ( 333 mm ) of precipitation was reported in a four @-@ day , accounting for a third of the station 's yearly average rainfall . Strong storm surge was reported at the same location . The waves swept boats away from the coasts of islands . Further inland , there was extensive damage to homes and crops , though no people died . Despite evidence that the system had distinct tropical characteristics , it was not operationally added to HURDAT .
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5796 = = = Hurricane Eight = = =
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5797 On October 19 , a low @-@ pressure area moved into the southwestern Caribbean Sea . The area of disturbed weather quickly became well @-@ organized , and was analyzed to have become a tropical depression at 0000 UTC on October 20 . Initially , the tropical cyclone moved very slowly towards the west and then the northwest . Shortly after formation , the disturbance intensified into a tropical storm at 1800 UTC later that day . The S.S. Cristobal provided the first indications of a tropical cyclone in the region , after reporting strong gusts and low pressures north of the Panama Canal Zone during that evening . Continuing to intensify , the storm reached hurricane intensity at 0600 UTC on October 22 . Several vessels in the storm 's vicinity reported strong gusts and rough seas generated by the storm . Later that day at 1200 UTC , the ship S.S. Castilla reported a minimum pressure of 983 mbar ( hPa ; 29 @.@ 03 inHg ) near the periphery of the storm . Based on this observation , the hurricane was estimated to have reached intensity at the same time with winds of 80 mph ( 130 km / h ) . The hurricane subsequently curved west and then southwest , before making its only landfall in northern Nicaragua at 1900 UTC on October 23 at peak intensity . Once inland , the tropical cyclone rapidly weakened over mountainous terrain , and dissipated at 1200 UTC the following day . Reports of damage were limited , though a report stated that considerable damage had occurred where the hurricane made landfall .
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5798 = = = Tropical Storm Nine = = =
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5799 On October 23 , an open trough was centered north of Hispaniola near the Turks and Caicos islands . At 0000 UTC the following day , the area of disturbed weather became organized and was analyzed to have become a tropical storm southeast of Inagua , based on nearby vessel reports . Initially , the storm drifted northward , but later began to accelerate towards the northeast after a roughly 12 @-@ hour period . At 0600 UTC on September 25 , the disturbance slightly gained in intensity to attain maximum wind speeds of 45 mph ( 75 km / h ) ; these would be the strongest winds associated with the storm as a fully tropical cyclone . A reanalysis of the system indicated that due to a lack of definite tropical features , the storm may have had been a subtropical cyclone . On October 26 , the system became increasingly asymmetric and had developed frontal boundaries , allowing for it to be classified as an extratropical cyclone at 0600 UTC that day . Once transitioning into an extratropical system , the storm continued to intensified as it moved northward . On October 27 , the system was analyzed to have a minimum pressure of at least 985 mbar ( hPa ; 29 @.@ 09 inHg ) after passing to the southeast of Bermuda . At 1200 UTC later that day , the cyclone reached an extratropical peak intensity with winds of 80 mph ( 130 km / h ) just east of Newfoundland . Had the storm been tropical at the time , it would have been classified as a modern @-@ day Category 1 hurricane . Subsequently , the extratropical storm curved eastward , where it persisted before dissipating by 1800 UTC on September 29 .