<\/p>\n
+ It lasted only 3 days, before wind shear<\/strong> caused it to die.\n<\/p>\n <\/p>\n + Barry quickly weakened after wind shear<\/strong> blew away most of the thunderstorms.\n<\/p>\n <\/p>\n + But a lot of wind shear<\/strong> gave Harvey some subtropical characteristics and also made the official forecasts to underestimate the future strength of the storm.\n<\/p>\n <\/p>\n + It reached its peak winds of 70mph, but wind shear<\/strong> and cooler waters quickly caused Peter to lose strength.\n<\/p>\n <\/p>\n + However, wind shear<\/strong> and dry air quickly weakened Omar to a minimal hurricane that afternoon as it raced towards the northeast at 26mph.\n<\/p>\n <\/p>\n + It moved usually west, and was later torn apart by wind shear<\/strong> on September 8.\n<\/p>\n + On the next day, wind shear<\/strong> around the storm caused it to weaken into a remnant low.\n<\/p>\n <\/p>\n + Early on August 3, strong wind shear<\/strong> over Chris removed the deep convection from the low level circulation, while a building ridge ridge to its north turned the storm towards the west into an area of drier air.\n<\/p>\n <\/p>\n + On November 2, wind shear<\/strong> started affecting the storm, and all convection was gone by the next day, when it was located roughly 520mi off the coast of Oregon.\n<\/p>\n <\/p>\n + Low amounts of wind shear<\/strong> and favorable outflow allowed strong deep convection to develop and persist near the center, and by 1800Coordinated Universal TimeUTC on September 2 the system developed into Tropical Depression Nine about 450miles southwest of Praia, Cape Verde.\n<\/p>\n <\/p>\n + Some fluids are anti-thixotropic: constant shear<\/strong> stress for a time causes an increase in viscosity or even solidification.\n<\/p>\n <\/p>\n + Wind shear<\/strong> caused Alex to die on August 2.\n<\/p>\n <\/p>\n + Intensification was partly suppressed by high wind shear<\/strong> and by cool sea surface temperatures in the wake of Hurricanes Gordon and Helene.\n<\/p>\n <\/p>\n + Steering currents pulled Ignacio north, where it encountered wind shear<\/strong> and cooler waters.\n<\/p>\n <\/p>\n + March was an inactive season, with only one tropical depression forming, Chedeng, which made landfall in Mindanao, before dissipating in the Sulu Sea, where wind shear<\/strong> was destructively high.\n<\/p>\n <\/p>\n + Favourable sea temperatures, low wind shear<\/strong> and excellent vertical outflow made the system intensify into a tropical storm, then the JMA named it “Vongfong”.\n<\/p>\n <\/p>\n + A small area of convection 600 miles southeast of Rio de Janeiro moved into an area of low wind shear<\/strong> and barely 26\u00b0C warm waters on February 23, 2006.\n<\/p>\n <\/p>\n + Despite wind shear<\/strong> values of about 30mph.\n<\/p>\n <\/p>\n + Wind shear<\/strong> finally caused Fay to weaken to a tropical storm later that day.\n<\/p>\n <\/p>\n + This is usually due to friction, though the use of shear<\/strong> force of the surface is also commonly used.\n<\/p>\n <\/p>\n + It briefly threatened the Hawaiian Islands near peak strength, but instead encountered wind shear<\/strong> and weakened.\n<\/p>\n <\/p>\n + Later that day, despite wind shear<\/strong> from powerful Hurricane Wilma nearby, it strengthened into a tropical storm as it moved west-northwestward.\n<\/p>\n <\/p>\n + The hurricane again re-intensified before cold air and wind shear<\/strong> penetrated the inner core of convection.\n<\/p>\n <\/p>\n + Like previous storms Tropical Storm Ingrid Ingrid and Karen, high wind shear<\/strong> in the deep tropics delayed Melissa’s development.\n<\/p>\n <\/p>\n + It was named on November 24, the storm moved west-southwest for several days, and wind shear<\/strong> caused it to weaken to a tropical depression on November 26.\n<\/p>\n <\/p>\n + The shear<\/strong> greatly lessened greatly on the 19th, and John became a hurricane on the 20th.\n<\/p>\n <\/p>\n + Ioke began to transition into an extratropical cycloneextratropical storm late on September 4 due to increased wind shear<\/strong> and rapidly cooling seas, and the JTWC issued its last advisory at 1200 UTC on September 5 after it was decided that Ioke had begun extratropical transition.\n<\/p>\n <\/p>\n + However, Chris began to be affected by strong wind shear<\/strong> and became disorganized.\n<\/p>\n <\/p>\n + Blows to the head can shear<\/strong> off the olfactory nerves that pass though the ethmoid bone and cause anosmia, an irreversible loss of the sense of smell and a great reduction in the sense of taste.\n<\/p>\n <\/p>\n + These characteristics were operationally recognized for three hours before high shear<\/strong> began to tear the system apart, just short of the six hours required to be officially declared a tropical depression.\n<\/p>\n <\/p>\n + These locks are more difficult to pick than warded locks and are picked by putting tension on the keyhole and pushing the pins or wafers up individually until they reach the shear<\/strong> line.\n<\/p>\n <\/p>\n + It was slow to become stronger at first, but on September 26, Karen quickly became stronger and was made a hurricane early in the day before added wind shear<\/strong> stopped the intensification and began to slowly weaken the storm.\n<\/p>\n <\/p>\n + On November 20, wind shear<\/strong> had destroyed Gamma and advisories were stopped, although the low level circulation of Gamma survived for an extra 36\u201348hours.\n<\/p>\n <\/p>\n + Nevertheless, an average shear<\/strong> stress is a reasonable approximation.\n<\/p>\n <\/p>\n + A strong ridge of high pressure over the Northeastern Pacific Ocean forced John westward, where upper level shear<\/strong> kept John a tropical storm as its intensity fluctuated.\n<\/p>\n <\/p>\n + A Newtonian fluid is a fluid, where the ratio between shear<\/strong> stress changes linearly in proportion to the stress it is exposed to.\n<\/p>\n <\/p>\n + Strong wind shear<\/strong> weakened the storm, and Debby dissipated on August 27 over the northern Atlantic Ocean.\n<\/p>\n <\/p>\n + On December 7, wind shear<\/strong> began to cause Hurricane Epsilon to weaken.\n<\/p>\n <\/p>\n + Wind shear<\/strong> slowed down development greatly.\n<\/p>\n <\/p>\n + The storm did not get stronger because of a very strong wind shear<\/strong> from a strong tropical upper tropospheric trough.\n<\/p>\n <\/p>\n + This normally happens if upper-level wind shear<\/strong> is too strong.\n<\/p>\n <\/p>\n + Faulting occurs when shear<\/strong> stress on a rock overcomes the forces which hold it together.\n<\/p>\n <\/p>\n + Vertical shear<\/strong> increased, weakening Mike to a tropical storm on the 16th.\n<\/p>\n <\/p>\n + Crevasses form as a result of the movement caused by the shear<\/strong> stress between two semi-rigid pieces of ice.\n<\/p>\n <\/p>\n + The depression slowly moved west, and wind shear<\/strong> stopped the storm from becoming much stronger.\n<\/p>\n <\/p>\n + However, a second system developing in the southwestern edge of the Caribbean began pushing wind shear<\/strong> onto the depression on November 14, then weakening the depression into a tropical low; advisories were then temporarily stopped.\n<\/p>\n <\/p>\n + Wind shear<\/strong> also caused in to die on September 2.\n<\/p>\n <\/p>\n + These macroscopic characteristics constitute the essential distinctions: a liquid flows, lacks a definite shape, and cannot withstand a shear<\/strong><\/strong> stress; a solid does not flow, has a definite shape, and exhibits elastic stiffness against shear<\/strong><\/strong> stress.\n<\/p>\n <\/p>\n + It can be used as either baby alpaca, which is the first shear<\/strong><\/strong> of an alpaca, or plain alpaca, which comes from subsequent shear<\/strong><\/strong>s.\n<\/p>\n <\/p>\n + Tropical Storm Ivan slowly became more organized as wind shear<\/strong> decreased, and its outflow expanded in all quadrants.\n<\/p>\n <\/p>\n + After several days, Florence encountered an area of lesser wind shear<\/strong> and strengthened into a hurricane on September 10.\n<\/p>\n <\/p>\n + Stated differently, a solid exhibits resistance to shear<\/strong> stress while a liquid does not.\n<\/p>\n <\/p>\n + Other Non-Euclidean geometry#Planar algebrasplanar algebras are used to represent the shear<\/strong> mapping of classical motion in absolute time and space and to represent the Lorentz transformations of relativistic space and time.\n<\/p>\n <\/p>\n + New stars are forming in the shear<\/strong> region.\n<\/p>\n <\/p>\n + Simultaneously, the trough in the upper troposphere weakened, causing the wind shear<\/strong> in the area to decrease, also allowing the new tropical depression to develop.\n<\/p>\n <\/p>\n + Upper level shear<\/strong> weakened the hurricane to a tropical storm on the 10th, and John became extratropical in the North Central Pacific about a thousand miles south of Unalaska Island.\n<\/p>\n <\/p>\n + As shear<\/strong> stayed low and the oceans stayed warm, Helene got a little bit stronger.\n<\/p>\n <\/p>\n + A joint does not involve shear<\/strong> displacement, and forms when tensile stress breaches its threshold.\n<\/p>\n <\/p>\n + Constant shear<\/strong> stress can be applied by shaking or mixing.\n<\/p>\n <\/p>\n + Franklin moved unevenly to the east while weakening as shear<\/strong> increased again.\n<\/p>\n <\/p>\n + It quickly lost strength because of wind shear<\/strong> and a close cold front.\n<\/p>\n <\/p>\n![\"shear](\"https:\/\/englishteststore.net\/blog\/wp-content\/uploads\/2021\/09\/shear-how-to-use.jpg\" "\\"shear")
Example sentences of “shear”:<\/h2>\n
+ On the next day, wind shear<\/strong> around the storm caused it to weaken into a remnant low.\r\n
+ Early on August 3, strong wind shear<\/strong> over Chris removed the deep convection from the low level circulation, while a building ridge ridge to its north turned the storm towards the west into an area of drier air.\r\n
<\/pre>\nMore in-sentence examples of “shear”:<\/h2>\n