Leclimatiseur mobile est doté d’une fonction optionnelle nommée silence, silent ou sleep. Pour l’activer, il suffit d’appuyer sur le bouton correspondant, via la télécommande ou le panneau de contrôle situé en façade. Le climatiseur se met alors à tourner au ralenti. Le compresseur en sous-régime devient plus discret. Putthem in place the same way you placed the upper support pieces, but 2” from the bottom of the legs.|Step 10: Take a 1” x 4” x 8’ piece of wood and, using a miter saw, cut two (2) 1” x 4” x 39” pieces. The actual size for these pieces will end up being around ¾”x 3 ½”x 39”.|These two pieces will be the outside pieces of the lower shelf of your wood coffee table. These Climatiseurmobile réversible EQUATION Top 3 3800 W Score global : 3,5 étoiles sur 5. 106 avis climatiseur mobile monobloc 2600w 30m² - livoo 549.00 € 334.52 € Vendu par Nouveaux Marchands. Livraison offerte . Climatiseur Mobile Electrique 900W 2300/8000 W/BTU 2 vitesses jusqu'à 30 m² CM 25 T.1 Splus 679.93 € Vendu par Outillage Online. Livraison offerte . Retourà la liste Accueil Petit Electroménager Confort de la maison Ventilateur et climatiseur Climatiseur mobile dolceclima silent 10 p - 2600w-8900 btu 01920 ol_01920. Climatiseur mobile dolceclima silent 10 p - 2600w-8900 btu 01920. OL_01920; Ce produit n'est plus disponible. Fermer. Description détaillée Caractéristiques Avis, Questions & Réponses. Description du Livoo- Climatiseur mobile connecté - 2600 W - Blanc. Programmable à distance avec l'application TUYA - Pour une surface jusqu'à 30 m² - 2 vitesses de ventilation - température réglable de 15 °C à 31 °C - Double Fonction déshumidification et ventilation. 329,99 €. Plus d'offres à partir de 329,99 €. Livraison gratuite. 0LGJ63. The Beaufort Wind Force Scale, The Saffir-Simpson Hurricane Scale, & the Fujita Scale of Tornado Intensity 0calm 1light airjust sufficient to give steerage breezeSufficient wind for working ship. 2light breezeThat in which a well-conditioned man-of-war with all sail set and "clean full" would go in smooth water from1 to 2 knots 3gentle breeze3 to 4 knots 4moderate breeze5 to 6 knotsmoderate breezeForces most advantageous for sailing with leading wind and all sail drawing. 5fresh breezeThat to which she could just carry in close "full and by"Royals, &c. 6strong breezeSingle-reefed topsails or topgallant windReduction of sail necessary even with leading wind. 7moderate/near galeDouble-reefed topsails, jib, &c. 8fresh gale/galeTriple-reefed topsails, & forcesConsiderable reduction of sail necessary even with wind quartering. 9strong galeClose-reefed topsails and courses. 10whole gale/stormThat which she could scarcely bear with close-reefed main topsail and reefed foresailstorm forcesClose reefed sail running, or hove to under storm sail. 11storm/violent stormThat which would reduce her to storm stay-sails 12hurricaneThat which no canvas could sail can stand even when running The Beaufort Scale has become the standard method of judging wind force. It is not the oldest, since rating the strength of wind by number and/or assigning names to the ratings had been done for some time. In 1806 Francis Beaufort later Admiral and Sir wrote out a numerical scale in his log. This was evidently copied from a British Admiralty pamphlet. Beaufort, however, refined and specified the scale, and in 1838 it was officially adopted by the Admiralty. In 1906 a report further refined the scale with corresponding wind speeds and descriptions of effects on land. Beaufort himself had specified the sailing conditions that went with each rating, as seen in the chart at right. Separate wind scales for tornadoes and hurricanes did not come until the 1970's. The Fujita or Fujita-Pearson Scale for tornadoes was proposed in 1971 by T. Theodore Fujita and Allen Pearson. Soon thereafter, the Saffir-Simpson Scale for hurricanes was formulated by Herbert Saffir and Robert Simpson. Thus, the movie Twister was anachronistic when it had Helen Hunt's father warn, in 1965, that they might have an F5 tornado headed toward them. The scale had not been invented yet. There has been some recent revision of some of these systems. I have not yet updated the presentation here. The complete Beaufort Scale has thirteen divisions, as shown above starting with zero. Beaufort grouped these into 5 categories of winds, or finely divided using five "breezes," four "gales," and four other designations. light gentle moderate fresh strong whole Breezes and gales both use the same simple scale of adjectives in the table at left. It always seemed a little odd to me that the designations jumped directly from "breezes" to "gales." One might expect an intermediate category, like simple "winds." Indeed, Beaufort himself grouped "strong breeze" and "moderate gale" as "strong winds" [note]. The Fujita and Saffir-Simpson scales are almost entirely subdivisions of hurricane force winds. Only the F0 tornado merely has gale force winds. The complete table below gives wind speeds, the appearance of objects affected by the wind as described in 1906, the kinds of damage to be expected from tornadoes and hurricanes, and other details, like barometric pressure, for hurricanes. Gale force winds mean that a "tropical depression" becomes a "tropical storm," which is then given a name by the appropriate authorities. Warning flags for water craft are also given. At the left of the table, the Beaufort, Fujita, and Saffir-Simpson Scales are given B, F, and S numbers, respectively. Note that severe hurricanes are often attended with tornadoes as well. Hurricanes in the Western Pacific are called "Typhoons," and those in the Indian Ocean, "Cyclones." Tornadoes used to often be called "Cyclones" also. Modern terminology is that all low pressures systems, which includes hurricanes, tornadoes, and less severe phenomena, are "cyclones." In 1927, a German captain, Petersen, provided "State-of-Sea" descriptions for each wind force. These are given at right. The term "white horses" is not familiar to me, at least from American usage. This seems to mean simply "whitecaps." B0Calm74 mphThe air is filled with foam and spray. Sea completely white with driving spray; visibility seriously affected. devastation occurs Hurricane Warning F1Tornado, Fujita Scale 173-112 mph roofs damaged; barns torn apart; weak trailers flipped and torn apart; cars thrown from roads; sheet metal buildings destroyed S1Category I Hurricane, Minimal74-95 mph barometer >= 980 mb hPa, inches; storm surge 4-5 ft damage primarily to shrubbery, trees, foliage, unanchored mobile homes, and small unsecured coverings carports. No significant damage to well anchored structures. Some damage to poorly constructed signs. Low lying coastal roads inundated. Minor pier and marina damage. Small craft exposed to open moorings may be torn free S2Category II Hurricane, Moderate96-110 mph barometer = 979-965 mb hPa, inches; storm surge 6-8 ft considerable damage to foliage and shrubbery, smaller trees uprooted. Major damage to exposed mobile homes. Extensive damage to poorly constructed signs. Possible damage to roofing, windows and doors. No major damage to secure buildings. Coastal roads and low-lying escape routes cut by rising waters 2 to 4 hours prior to storm arrival. Considerable damage to piers. Marinas flooded by storm surge. Small craft in open moorings ripped free from mooring. Evacuation of low-lying areas and shoreline residences required Alma, 06/08/66, 110 mph, 970 mb S3Category III Hurricane, Extensive111-130 mph barometer = 964-945 mb hPa, inches; storm surge 9-12 ft foliage torn from trees; large trees blown down. Practically all poorly constructed signs destroyed. Some damage to roofing and windows that are unbraced. Mobile homes unsecured destroyed. Serious flooding of coastal areas and smaller buildings destroyed along shoreline; larger structures near coast damaged by battering waves and debris. Low-lying escape routes cut by rising water inland 3 to 5 hours before hurricane center arrival. Terrain continuously lower than 5 ft above mean sea level may flood as much as 8 miles or more inland. Evacuation of shoreline and low-lying surrounding area where hurricane is estimated to come ashore may be required to be evacuated Bob, 08/19/91, 115 mph, 953 mb F2Tornado, Fujita Scale 2113-157 mph strongly built schools, homes, and businesses unroofed; concrete block buildings, weak homes, and schools destroyed; trailers disintegrated S4Category IV Hurricane, Extreme131-155 mph barometer = 944-920 mb hPa, inches; storm surge 13-18 ft shrubs and trees uprooted; all signs blown down or destroyed. Extensive damage to roofing, windows, and doors. Complete failure of roofs on smaller structures. Complete destruction of mobile homes whether secured or not. Terrain continuously lower than 10 feet above mean sea level may flood requiring massive evacuation of residences as far as 6 miles or more inland. Major damage to lower floors of large structures near shore line due to flooding and debris. Low-lying escape routes will be cut off 3 to 5 hours prior to hurricane center arrival due to flooding from storm surge. Major erosion of beachheads and coastal formations David, 08/30/79, 150 mph, 924 mb Hugo, 09/15/89, 140 mph, 918 mb Andrew, 08/23/92, 150 mph, 922 mb S5Category V Hurricane, Catastrophic>155 mph barometer 18 ft shrubs and trees blown down and uprooted; considerable damage to roofs of all buildings; all signs down. Very severe and extensive damage to windows and doors. Complete failure of roofs on several residences and industrial buildings. Extensive shattering of glass from pressure variation and blown debris. Some complete building failures. Smaller buildings are overturned or destroyed. Complete destruction of mobile homes. Major damage to lower floors of large structures less than 15 ft above sea level within 750 yards of shore. Low-lying escape routes cut off due to flooding 6 to 8 hours prior to hurricane center arrival. Massive evacuation of residential areas on low-lying ground within 5 to 10 miles of shore may be required with possible extension up to 15 miles inland Camille, 08/18/69, 165 mph, 909 mb Gilbert, 09/14/88, 160 mph, 888 mb F3Tornado, Fujita Scale 3158-206 mph strongly built schools, homes, and businesses have outside walls blown away; weaker homes completely swept away F4Tornado, Fujita Scale 4207-260 mph strongly built homes have all interior and exterior walls blown apart; cars thrown 300 yards or more in the air F5Tornado, Fujita Scale 5"finger of God"261-318 mph strongly built homes are completely blown away My introduction to meteorology came with the Life Science Library book Weather, by Philip D. Thompson, Robert O'Brien, and "the Editors of LIFE" [Time Incorported, 1965], which I acquired, about the time it was published, when I was in Junior High School. Some of the descriptions here are still drawn from that volume. I did have an actual meterology class at the University of New Mexico in 1968, but I got less out of it than I might have and failed to hold on to any class materials. Now, however, complete background to all of this can be found at The Weather Channel website. The following descriptions have been taken from that source, from Everything Weather, The Weather Channel's CD-ROM, and from other sources, web and print, that I have lost track of. A detailed history of the Beaufort Scale is now to be found in Defining the Wind, The Beaufort Scale, and How a 19th-Century Admiral Turned Science into Poetry by Scott Huler [Three Rivers Press, New York, 2004]. I was unaware of the sailing condition descriptions, or indeed of the history of the Scale, until finding this book. The Petersen State-of-Sea descriptions can be found at the British Meterological Office. Masts and Sails Clouds Note on Dew Point Snow, Sleet, Ice, and Rain Philosophy of Science, Meteorology Philosophy of Science Home PageCopyright c 1998, 2006, 2008, 2019 Kelley L. Ross, All Rights Reserved The Beaufort Wind Force Scale, Note 0calm 1light air 2light breeze 3gentle breeze 4moderate breeze/breeze 5fresh breezemoderate wind 6strong breezefresh wind/wind 7moderate/near galestrong wind 8fresh gale/gale 9strong gale 10whole gale/storm 11storm/violent storm 12hurricane It may be silly, but it bugs me that the Beaufort terminology should jump directly from a "breeze" to a "gale." As I use the words, "wind" can refer to all movement of air, but the very same word also denotes something that is rather more than a "breeze" but still less than a "gale." I don't think of a breeze as much of a wind at all, while a gale is something quite strong and unusual, at least on land, or apart from a winter storm. A breeze is pleasant, and will not cause any inconvenience or rearrange any objects, except the lightest. A real wind, however, many be annoying, render some activities unpleasant, and will move some things around, even if only leaves, that will require attention. But then a gale no outside activities will be pleasant, and the wind can cause some damage. I remedy this with the additions at left. Here we simply would have three "breezes," three "winds," and three "gales." This is how it might be done in Chinese, where many things, like rank, are divided into "high," , "middle" , and "low" , degrees. I expect that the exclusive use of "breeze" and "gale," without using "wind" for specific forces, might be to avoid ambiguity. In the traditional Beaufort Scale "wind" is not used with two meanings, the general and the specific. That is quite reasonable. My proposal then, would certainly not be for any usage where ambiguity might cause some inconvenience or danger. The table simply represents my intuition about ordinary usage and meaning, that a breeze is not quite a wind, while a gale is much more than just a wind. Return to Text Clouds Clouds are the mountains of the sky. They can, indeed, be taller than any mountains of the earth, reaching up to 40,000 feet or, rarely, even to 60,000 feet, far beyond Everest. On the other hand, they exist on a vastly different time scale. The tallest clouds can develop and disappear in less than a day, while earthly mountains grow and erode over millions of years. In Los Angeles, there is usually not much to be seen in the way of interesting clouds. Much of the weather is simply clear, and in the spring and summer a marine layer of fog and stratus clouds moves in. Occasionally in the summer, thunderheads develop over the San Gabriel mountains and the storms may, though sometimes not for several years, move over the Los Angeles basin. Winter storms off the Pacific, usually lasting no more than a day or two, are responsible for most of the average rainfall of 15 inches. Growing up in Los Angeles, I didn't feel like I saw much in the way of cloud variety until I lived in New Mexico, Lebanon, Hawaii, and Texas. New Mexico was especially noteworthy for the colors that would play on the clouds The setting sun could fill the same sky with yellow, pink, orange, and cherry red on different clouds. In Hawaii, where clouds would build up over the windward mountains daily in the rainy season, one striking memory is of the full moon shining on the towering, isolated thunderheads. There was, however, limited thunder from those clouds, which would drop some rain in the valleys and foothills and then disperse, often not even getting Waikiki wet. More violent weather came with the occasional winter storm a "kona" storm, since the wind may blow from leeward, against the trade winds, or with the rare hurricane. Clouds are classified by form and by altitude. The basic forms, with symbols, are "heaped up," in Latin, "spread out," the neuter form of which is stratum, used for extensive layers of similar rock in geology, and "lock" or "curl" of hair. Cumulus clouds tend to form from rising air, from 6,000 feet on up, and so are classified as "vertically developing" clouds. Stratus clouds, below 8,000 feet, may be rather like an elevated fog bank; or, altenatively, fog can be thought of as a stratus cloud at ground level. While cumulus clouds mean that air has risen to an elevation where the temperature is at the dew point, so that the water condenses, with stratus clouds the temperature of the air itself may have fallen to the dew point. Cirrus clouds are ice crystals at high altitude, from 18,000 to 40,000 feet; their whispy structure comes from scattering by the wind. Besides stratus, low level clouds can include between 3,000 and 10,000 feet, from which rain falls nimbus simply means "cloud," or "raincloud" and below 8,000 feet, where cumulus clouds stretch out in a solid layer, showing a lot more structure than stratus clouds, whose outlines can be very indistinct. At high altitudes 18,000 to 40,000, cirrus clouds can form a fairly solid layer, becoming , or they can take on a lumpy structure, with grains or ripples a "mackerel sky", suggestive of cumulus clouds, becoming . At middle altitudes, from 6,000 to 18,000 feet, too low to freeze into cirrus but higher than ordinary stratus, are above 15,000 feet and . The "alto-" element is from Latin "altus," which originally meant "grown" but came also to mean "high," as it is used in these names. Altocumulus can be part of the development of cumulus and cumulonimbus clouds. The highest - all the way up to 60,000 feet - most spectacular, and most violent clouds result when the air, rising to form cumulus clouds, continues to rise, drawing moisture to high altitudes and generating extreme conditions. This makes a cumulonimbus cloud. The swelling top spreads out into a characteristic anvil shape, which then may be blown away by high level winds. Because of freezing air at those altitudes, the streaming clouds from the anvil will often take a cirrus form. Freezing air can also cause hail to form, as ice crystals begin to fall and then are lifted back up again and again to grow larger and larger. When the hail finally falls, descriptions of its size are borrowed from the produce counter and from sports Small hail is described as "pea" sized, whence we move up to "grape" sized, "ping-pong ball" sized, "golf ball" sized, "baseball" sized, and, most devastating of all, "grapefruit" sized. Baseball and grapefruit sized hail can break any window, ruin a car, flatten a field of crops, or even kill somebody. The movement of wind, water, and ice up and down the column of clouds also generates differentials in electrical charge, which are then discharged as lightning. Isolated thunderstorms, generated by summer heating, may pass over with a minimum of damage. Spring cold fronts, however, pushing still cold air from the north under warm moist Gulf air, as in Texas, can produce massive squall lines of thunderstorms, stretching for hundreds of miles, filling the sky with vast gray clouds, rain, wind, hail, lightning, and, worst of all, tornadoes. These conditions get called, with charming understatement, "severe weather." Short of hurricane force winds, or actual tornadoes, nature provides no more awesome weather. During one overnight thunderstorm and flash flood that I witnessed in Austin, Texas, on the eve of Memorial Day in 1981, where serious flooding and deaths occurred, the flashes of lightning were so frequent that they were right on top of each other and the night was literally without darkness. I also see other cloud symbols, such as the altostratus plus cirrus symbol at left. I have yet to see exactly what this would look like in the sky, but I like how this looks. The Beaufort Wind Force Scale, The Saffir/Simpson Hurricane Scale, & the Fujita Scale of Tornado Intensity Note on Dew Point Snow, Sleet, Ice, and Rain Philosophy of Science, Meteorology Philosophy of Science Home PageCopyright c 1998, 2015 Kelley L. Ross, All Rights Reserved Note on Dew Point The dew point tells us the absolute humidity. The more commonly used "relative humidity" is the percentage to which the air is saturated with moisture. The dew point is simply the temperature at which the air would be saturated, would have 100% relative humidity. Warmer air can hold more moisture, so that air that would be saturated at 75oF, with 100% relative humidity, would only have about 50% relative humidity if the temperature rises to 95oF without any moisture being added. While people complaining of summer humidity often say that both the temperature and the relative humidity must both be 90 or more, this really does not happen and would be deadly if it did. Typical summer dew points in Texas are around 75oF, as in the example just cited. The highest dew point I've ever heard of was 80o, reported by The Weather Channel at places in eastern Pennsylvania and New Jersey as a line of thunderstorms was arriving in June 1998 I was nearby in New Jersey - it was humid. Typical summer dew points in Los Angeles are in the 50's. Extremely humid summer conditions in Los Angeles usually only mean dew points in the 60's. Autumn arrives in Los Angeles in October, when dry air and sometimes a Santa Ana wind arrives with the first cold front, dropping the dew point precipitously. October 20, 1996, the dew point in Van Nuys was reported at 37o, the 21st at 14o, and the 22nd at 9o. October 7, 1997, the dew point was reported at 39o and the 15th at 25o. October 5, 1998, the dew point was reported at 13o and the 17th at 19o. Although understanding the dew point in abstraction, its real connection to the feel of the air was not obvious to me until I began seeing dew point isotherm maps on The Weather Channel in the 1980's. Since air can hold about twice as much moisture for every 20 degrees Fahrenheit, this may be used to write very simple equations for the dew point. In the following equations, D is the dew point in degrees Fahrenheit, T is the air temperature, and H is the relative humidity written as a whole number percentage "50" instead of " for "50%". The first equation gives the dew point for the temperature and relative humidity, which is usually what one can easily determine, while the second equation gives the relative humidity from the temperature and dew point. D = T - 20*2 - log H/log 2 log H = 2 - log 2*T-D/20 C = 5*F - 32/9 C = 5*F + 40/9 - 40 F = 9*C/5 + 32 F = 9*C + 40/5 - 40 A more precise value for the dew point can be derived from the equations below. For the main equation, the value "X" must be calculated first, based on the relative humidty. The temperature and dew point here will be in degrees Celsius or centigrade. Celsius and Fahrenheit can be converted back and forth with the equations in the box at right. Note that the equations that add and subtract 40, in precisely the same way, may be easier to remember than the more traditional conversion equations. X = 1 -.01*H D = T - - - If we have a temperature of 73oF at 24% relative humidity, the Fahrenheit equation gives us a dew point of The Celsius equation gives us a dew point of or An error of or is not bad, especially considering how much easier the Fahrenheit equation is to use. My favorite personal experience with dew point was when I drove from Austin, Texas, to Tularosa, New Mexico, in June 1982. A cold drink in Texas causes a large amount of moisture to condense on a glass. It "sweats"; and the water collects on the table or in a coaster, sometimes so much that it makes it seem like the glass is leaking. Arriving in New Mexico at my aunt and uncle's place, the next day I had a glass of iced tea sitting on the broad arm of a wooden chair. After half an hour, I checked the glass to make sure that there wasn't any condensing water that might damage the wood. There wasn't. At an elevation of over 4000 feet, far from the Gulf Coast, the relative humidity might only have about 5% or so. Return to "Clouds" Philosophy of Science Home PageCopyright c 1998 Kelley L. Ross, All Rights Reserved Snow, Sleet, Ice, and Rain The temperatures of the air produce different phenomena of precipitation. The most familiar are snow and rain. In the former, ice crystals fall through air that is below freezing from the clouds to the surface. Snow then accumulates in drifts on the ground. The water content of snow can vary, so that some times it is dry, light, and fluffy, other times wet, heavy, and dense. Wet snows can adhere, so that drifts can appear to flow or sag without breaking apart. With rain, water droplets fall through air that is above freezing. Puddles accumulate on the ground, or the water flows away. Other forms of precipitation occur when the air temperature changes from above freezing to below between the clouds and the surface. If the boundary occurs high enough, there is time for rain droplets to freeze before hitting the ground. This is sleet. As solid little ice pellets, sleet will tend to fall faster than snow and will hit surfaces with some noise. A snow fall is silent. Sleet can sound like small hail. When it accumulates on the ground, sleet can look a bit like snow, but the consistency and the color will look a bit different. If the boundary between the air above freezing and below freezing is close enough to the surface, we get freezing rain. This is one of the rarer of these phenomena, and its effects are striking and dangerous. Rain drops hit surfaces and freeze. This produces a glaze of ice on amost anything and a surface of "black" ice on streets. An accumulation of ice becomes heavy. Branches, trees, and power lines can easily be brought down in an ice storm. Driving is treacherous. Some of the dangers involved can be seen in the Ang Lee movie The Ice Storm [1997], where the weather ends up being incidental and symbolic with the tragic ending of the movie left rather hanging. In the daylight after an ice storm, everything looks like it is wrapped in glass. This can be extraordinarily beautiful, but it may be purchased at a terrible price in damage and even lives. Hail is produced when updrafts carry rain drops high into clouds, and into freezing air at altitude, even during warm times of the year. The rain drop freezes and may fall, or it may be carried up into the clouds again and receive a further coating of ice. This can happen over and over again, producing ever larger hail stones. Hail is thus usually characterized by its size, ranging from pea sized to grapefruit sized. The latter, of course, can cause sever damage or injury when it finally falls to the ground. I never saw more than the rare pea sized hail in Los Angeles, but I also got caught in heavy hail on I-90 outside Chamberlain, South Dakota, in July 2010, which dented my car, although not nearly as bad as with some cars I've seen. Some of the hailstones on that occasion seemed to be golf-ball sized. Snowfall is measured by its depth, but what that depth will be is variable relative to temperature and humidity. Thus, if snow is falling into air slightly above freezing, such as at 34oF, what would have been an inch of rain will result in seven inches of "wet" snow a 71 ratio. Wet snow can have a spectacular look, since, as noted above, it will tend to cling to branches and pile on narrow walls, can sag or flow off the walls or from steep surfaces, like roofs, and hang in waves or tongues that seem to defy gravity. At freezing, the snow is drier and will accumulate at about ten inches for an inch of rain 101. Colder temperatures mean drier snow yet, so that at 28o we get more like fiften inches of powdery snow for an inch of rain 151. Wet snow, of course, is also heavier, which is more of a strain for shoveling. I've also experienced the phenomenon, trying to dig out a car, that wet snow with above freezing temperatures, which melts a bit and then perhaps freezes overnight, produces a hard layer of ice, which may need to be broken before shoveling is even possible. I didn't need to worry about things like that when I was a resident of Los Angeles. The Beaufort Wind Force Scale, The Saffir/Simpson Hurricane Scale, & the Fujita Scale of Tornado Intensity Clouds Note on Dew Point Philosophy of Science, Meteorology Philosophy of Science Home PageCopyright c 2007, 2018 Kelley L. Ross, All Rights Reserved Sixteen short stories in the public domain, gathered from magazines, newspapers and the like 1 The Inconsiderate Waiter / J. M. Barrie 2 The Dead Sexton / Sheridan Le Fanu 3 The Demon Spell / Hume Nisbet 4 Romance of a Balloon / Hume Nisbet 5 A World of Sound / Olaf Stapledon 6 The Ghost-Ship / Richard Middleton 7 The Red Raid / Clarence Herbert New 8 Seaweed / Elia W Peattie 9 The Jerusalem Express / William J. Makin 10 Good Graft / Ellis Parker Butler 11 The Hunting of the Haggis / Guy Gilpatric 12 Climbing Death / Raoul Whitfield 13 Soaked in Seaweed / Stephen Leacock 14 Captain Cut-Throat / Albert Richard Wetjen 15 An Error in Equation / Ernest M Poate 16 False Teeth / Ernest M. Poate Cumulative Index   About Store Servers A place to hang out with like minded people and roleplay. Own and live in amazing houses, drive cool vehicles and explore the city. Be whoever you want to be in Brookhaven RP. Thanks for playing! Info Under desk buttons in Hospital, Police, Fire and Mayor were unintentionally working on 8/5. Please disregard desk buttons in this update. 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