From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #4235 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Wednesday, May 27 2020 Volume 14 : Number 4235 Today's Subjects: ----------------- Make American Great Again! ["Trump Golf Ball!" ] Interested in singles See photos! ["Colombian Woman" Subject: Make American Great Again! Make American Great Again! http://maskprotect.guru/4EerGo5MLNqDZzLk2UdsTJ9o43snzVEYpgaHo-_WDhxpp-Jy http://maskprotect.guru/1N7QYVqrVSIamTClQhTFdzxU5CM4ukxqHBXlnRVsQImLiJp7 Synoptic scale meteorology predicts atmospheric changes at scales up to 1000 km and 105 sec (28 days), in time and space. At the synoptic scale, the Coriolis acceleration acting on moving air masses (outside of the tropics) plays a dominant role in predictions. The phenomena typically described by synoptic meteorology include events such as extratropical cyclones, baroclinic troughs and ridges, frontal zones, and to some extent jet streams. All of these are typically given on weather maps for a specific time. The minimum horizontal scale of synoptic phenomena is limited to the spacing between surface observation stations. Global scale Annual mean sea surface temperatures. Global scale meteorology is the study of weather patterns related to the transport of heat from the tropics to the poles. Very large scale oscillations are of importance at this scale. These oscillations have time periods typically on the order of months, such as the MaddenbJulian oscillation, or years, such as the El NiC1obSouthern Oscillation and the Pacific decadal oscillation. Global scale meteorology pushes into the range of climatology. The traditional definition of climate is pushed into larger timescales and with the understanding of the longer time scale global oscillations, their effect on climate and weather disturbances can be included in the synoptic and mesoscale timescales predictions. Numerical Weather Prediction is a main focus in understanding airbsea interaction, tropical meteorology, atmospheric predictability, and tropospheric/stratospheric processes. The Naval Research Laboratory in Monterey, California, developed a global atmospheric model called Navy Operational Global Atmospheric Prediction System (NOGAPS). NOGAPS is run operationally at Fleet Numerical Meteorology and Oceanography Center for the United States Military. Many other global atmospheric models are run by national meteorological agencies. Some meteorological principles Boundary layer meteorology Boundary layer meteorology is the study of processes in the air layer directly above Earth's surface, known as the atmospheric boundary layer (ABL). The effects of the surface b heating, cooling, and friction b cause turbulent mixing within the air layer. Significant movement of heat, matter, or momentum on time scales of less than a day are caused by turbulent motions. Boundary layer meteorology includes the study of all types of surfacebatmosphere ------------------------------ Date: Wed, 27 May 2020 05:20:26 -0400 From: "Christopher" Subject: How To Build Your Own Military-Grade Silencer At Home (100% legal) How To Build Your Own Military-Grade Silencer At Home (100% legal) http://cleanpro.guru/KRYnTZe7_CkBChXJZGXmMAIb8BvBh9sMHQdlvUuVZAc6ufu_ http://cleanpro.guru/EBV4DAFD07JGE1UyPAr6sIpJzzE3cY3XFUPRDA_6Qs_Nso9L Although weather forecasts and warnings are the best known products of meteorologists for the public, weather presenters on radio and television are not necessarily professional meteorologists. They are most often reporters with little formal meteorological training, using unregulated titles such as weather specialist or weatherman. The American Meteorological Society and National Weather Association issue "Seals of Approval" to weather broadcasters who meet certain requirements but this is not mandatory to be hired by the medias. Equipment Satellite image of Hurricane Hugo with a polar low visible at the top of the image Main article: Meteorological instrumentation Each science has its own unique sets of laboratory equipment. In the atmosphere, there are many things or qualities of the atmosphere that can be measured. Rain, which can be observed, or seen anywhere and anytime was one of the first atmospheric qualities measured historically. Also, two other accurately measured qualities are wind and humidity. Neither of these can be seen but can be felt. The devices to measure these three sprang up in the mid-15th century and were respectively the rain gauge, the anemometer, and the hygrometer. Many attempts had been made prior to the 15th century to construct adequate equipment to measure the many atmospheric variables. Many were faulty in some way or were simply not reliable. Even Aristotle noted this in some of his work as the difficulty to measure the air. Sets of surface measurements are important data to meteorologists. They give a snapshot of a variety of weather conditions at one single location and are usually at a weather station, a ship or a weather buoy. The measurements taken at a weather station can include any number of atmospheric observables. Usually, temperature, pressure, wind measurements, and humidity are the variables that are measured by a thermometer, barometer, anemometer, and hygrometer, respectively. Professional stations may also include air quality sensors (carbon monoxide, carbon dioxide, methane, ozone, dust, and smoke), ceilometer (cloud ceiling), falling precipitation sensor, flood sensor, lightning sensor, microphone (explosions, sonic booms, thunder), pyranometer/pyrheliometer/spectroradiometer (IR/Vis/UV photodiodes), rain gauge/snow gauge, scintillation counter (background radiation, fallout, radon), seismometer (earthquakes and tremors), transmissometer (visibility), and a GPS clock for data logging. Upper air data are of crucial importance for weather forecasting. The most widely used technique is launches of radiosondes. Supplementing the radiosondes a network of aircraft collection is organized by the World Meteorological Organization. Remote sensing, as used in meteorology, is the concept of collecting data from remote weather events and subsequently producing weather information. The common types of remote sensing are Radar, Lidar, and satellites (or photogrammetry). Each collects data about the atmosphere from a remote location and, usually, stores the data where the instrument is located. Radar and Lidar are not passive because both use EM radiation to illuminate a specific portion of the atmosphere. Weather satellites along with more general-purpose Earth-observing satellites circling the earth at various altitudes have become an indispensable tool for studying a wide range of phenomena from forest fires to El NiC1o. ------------------------------ Date: Wed, 27 May 2020 04:12:03 -0400 From: "**Live Show Latin**" <**LiveShowLatin**@maskprotect.guru> Subject: Find Attractive Latin Girls Here Find Attractive Latin Girls Here http://maskprotect.guru/9PbZhpC7iidKWOOr53bECLzmlswf3dfaSTXWeZSScT57EUPC http://maskprotect.guru/RMQXDEN7DB63G-HPbEiYPTlGh_0lV76iMPDsULDXODhMUndG Mawson's Far Eastern Party left on 10 November, and made good distances when weather allowed. By 14 December, they had travelled more than 480 kilometres (300 mi) towards Oates Land. Shortly after noon, as Mawson paused to calculate latitude, he saw that Mertz had stopped and was looking behind him. There was no sign of Ninnis. Mawson and Mertz retraced their steps and found a crevasse about 3.4 metres (11 ft) across; tracks on the far side made it clear that Ninnis, with his sledge and dogs, had fallen into the depths. Far below on a ledge, they could see the bodies of two dogs, and debris from the sledge, but no sign of Ninnis. Their remaining ropes were far too short to reach even the first ledge which they measured to be at a depth of 46 metres (150 ft), so they had no option except to hope that Ninnis would answer their shouts. They spent several hours calling but b having received no response b they were forced to give him up for dead. Shocked at the sudden loss of their companion, Mawson and Mertz now had to consider their own prospects. Ninnis's sledge had been carrying most of their provisions and equipment, and all of the dog food, leaving them with about 11 or 12 days' rations. To reach base they would have to augment these meagre supplies by shooting and eating the surviving dogs. They travelled steadily over the next days, despite Mawson suffering from snow-blindness; by 25 December, they calculated that they were 254 kilometres (158 mi) from Cape Denison. On 29 December, they killed the last of the dogs. Both men had been feeling unwell, but from New Year's Day 1913 there was a sudden and rapid deterioration in Mertz's health; he had frost-bite and became delirious and agitated.[n 7] After a weather delay, they resumed their journey on the evening of 3 January, but they did not get far before the weather and Mertz's frostbite forced them to stop. They laid up until 3 January when Mertz agreed to push on, but his condition continued to worsen and though Mawson managed to drag him on the sledge they could not cover much ground. Mertz died early on 8 January. Mawson was around 160 kilometres (100 mi) from the base, which was, he observed, a relatively short distance for a healthy man, but a long way for one weak and famished.[n 8] After burying Mertz and marking his grave, Mawson prepared for the journey ahead. To lighten his burden he used a small pocket tool to cut his sledge in half. On 11 January, the weather cleared and he set out. His extreme weakness and, in particular, the condition of his feet, meant he could not travel great distances. On 17 January, he fell into a crevasse and hung there by a rope from the sledge, which fortunately did not fall. It took him more than four hours to extricate himself. As he drew nearer to the base, he was frustratingly delayed by more bad weather. On 29 January he discovered a cairn, left by a search party, with food and a message telling him he was 37 kilometres (23 mi) from Aladdin's Cave. Three days later, Mawson reached the cave, where he discovered more provisions, but bad weather meant he could not set out again until 8 February. As he descended the final slope towards the base, he thought he saw smoke on the horizon, which he took to be coming from the departing ship. When he arrived at the base, he found that the ship had indeed sailed, earlier that day, leaving a group of five b Bickerton, Bage, Madigan, Alfred Hodgeman and Archibald McLean b and a new wireless technician, Sidney Jeffryes, as a rescue party for the missing men. Mawson radioed the ship, asking Davis to return and pick up the party; Davis attempted to comply, and brought the ship back to Commonwealth Bay, but a severe gale prevented the ship from anchoring or launching a boat. After sitting offshore for a day and worried that with further delays, Aurora would not reach Wild's western base before being blocked by winter ice, Davis gave up and headed west, leaving the Cape Denison group to spend another year at the ------------------------------ Date: Wed, 27 May 2020 06:02:02 -0400 From: "Trump Bill" Subject: Unique collector item or gift Unique collector item or gift http://resurge.guru/9sUrzxJJQI29AWhXi2qGISO6g9g3LKDWabBjquMYHf685PKI http://resurge.guru/kUH_q6KtLBL6p6JA-IPVnIo-sILeN8gaYz7P1G92PgmtSob9 The mesosphere is the third highest layer of Earth's atmosphere, occupying the region above the stratosphere and below the thermosphere. It extends from the stratopause at an altitude of about 50 km (31 mi; 160,000 ft) to the mesopause at 80b85 km (50b53 mi; 260,000b280,000 ft) above sea level. Temperatures drop with increasing altitude to the mesopause that marks the top of this middle layer of the atmosphere. It is the coldest place on Earth and has an average temperature around ?85 B0C (?120 B0F; 190 K). Just below the mesopause, the air is so cold that even the very scarce water vapor at this altitude can be sublimated into polar-mesospheric noctilucent clouds. These are the highest clouds in the atmosphere and may be visible to the naked eye if sunlight reflects off them about an hour or two after sunset or a similar length of time before sunrise. They are most readily visible when the Sun is around 4 to 16 degrees below the horizon. Lightning-induced discharges known as transient luminous events (TLEs) occasionally form in the mesosphere above tropospheric thunderclouds. The mesosphere is also the layer where most meteors burn up upon atmospheric entrance. It is too high above Earth to be accessible to jet-powered aircraft and balloons, and too low to permit orbital spacecraft. The mesosphere is mainly accessed by sounding rockets and rocket-powered aircraft. Stratosphere Main article: Stratosphere The stratosphere is the second-lowest layer of Earth's atmosphere. It lies above the troposphere and is separated from it by the tropopause. This layer extends from the top of the troposphere at roughly 12 km (7.5 mi; 39,000 ft) above Earth's surface to the stratopause at an altitude of about 50 to 55 km (31 to 34 mi; 164,000 to 180,000 ft). The atmospheric pressure at the top of the stratosphere is roughly 1/1000 the pressure at sea level. It contains the ozone layer, which is the part of Earth's atmosphere that contains relatively high concentrations of that gas. The stratosphere defines a layer in which temperatures rise with increasing altitude. This rise in temperature is caused by the absorption of ultraviolet radiation (UV) radiation from the Sun by the ozone layer, which restricts turbulence and mixing. Although the temperature may be ?60 B0C (?76 B0F; 210 K) at the tropopause, the top of the stratosphere is much warmer, and may be near 0 B0C. The stratospheric temperature profile creates very stable atmospheric conditions, so the stratosphere lacks the weather-producing air turbulence that is so prevalent in the troposphere. Consequently, the stratosphere is almost completely free of clouds and other forms of weather. However, polar stratospheric or nacreous clouds are occasionally seen in the lower part of this layer of the atmosphere where the air is coldest. The stratosphere is the highest layer that can be accessed by jet-powered aircraft. ------------------------------ Date: Wed, 27 May 2020 04:19:06 -0400 From: "Colombian Woman" Subject: Interested in singles See photos! Interested in singles See photos! http://cleanpro.guru/QLUPVQPR8iZzgP2ruumljnC7SRsypWWxHKB4_xhJk7kutyjj http://cleanpro.guru/FWGIv5Rn3PyEIXa1iuygtgwhioHbk0UreRez09RW2dMKNpzD For the group left at Cape Denison, winter came early, confining them mostly to the hut for many months. The previous year's program of magnetic and meteorological observations was resumed, as were the routines of daily life at the base. Many of the group found they had time on their hands, and McLean, in the tradition of earlier expeditions, took advantage of this to edit and produce a magazine, the Adelie Blizzard. One major improvement on the previous year was that, from 20 February, regular wireless contact with Macquarie Island was established, which allowed the group to stay in touch with the outside world until 8 June, when strong winds once again brought down the wireless masts. The wireless operator, Jeffryes, was initially a conscientious and respected member of the group, but from mid-June his behaviour began to deteriorate. He became moody and aggressive, challenging his hut mates to fights, mumbling to himself, developing a persecution mentality and neglecting his personal hygiene. This was alarming enough for the rest of the group, but when the wireless masts were re-erected early in August, Jeffryes began sending out wild messages, claiming that all the others apart from Mawson had gone insane and were trying to murder him. Bickerton began practising operating the wireless, and Mawson sent a message to Ainsworth at the Macquarie Island wireless station to censor all communications received from Jeffryes. Finally, in a period of semi-lucidity, Jeffryes asked to be relieved from his duties, and Bickerton permanently took over the wireless operator's role. As the weather was improving, Mawson decided that he would take out a final sledging party with Madigan and Hodgeman, primarily to recover equipment that had been dumped or cached during the journeys of the previous year. In this they were largely unsuccessful. They returned to base on 12 December and Aurora arrived the next day. They finally left Cape Denison on 24 December 1913. As they sailed away, they could see the cross, erected on high ground by Bickerton and McLean, commemorating their lost comrades, Ninnis and Mertz. Western base Frank Wild (left), leader of the Far Western Party, with Andrew Watson during the sledging expedition Mawson had hoped to place the western base around 800 kilometres (500 mi) (and no more than 970 kilometres (600 mi)) west of Cape Denison, to make inter-base wireless communication possible. After landing the Cape Denison party in January 1912, Aurora sailed west, well beyond the 800-kilometre (500 mi) mark, without finding any suitable landing spot. On 15 February, they were 2,410 kilometres (1,500 mi) from Cape Denison, and in danger of being frozen in for the winter when they found a large ice shelf at 66B0 21? S, 94B0 51? E. Lacking other options, Wild investigated it as a site for the base and, despite the possibility of the ice breaking up, he decided to risk it. The base was established by 21 February, when Aurora sailed for Hobart. Wild named the ice shelf after Shackleton, whose birthday fell on 15 February. Attempts to establish wireless contact with Cape Denison failed; they were unable to erect a suitable mast and discovered that vital parts of the transmitting equipment ------------------------------ Date: Mon, 25 May 2020 07:55:44 -0400 From: "African Grape" Subject: Does This African Witch Doctor Hold The Cure For Obesity? Does This African Witch Doctor Hold The Cure For Obesity? http://remegrow.bid/au9s6v4egzcs1zoVbXcfBVkxjDong0GanAmdaHUfxg7xZkw http://remegrow.bid/vQlFKvEZL6DaIA8TSJqtXIePA2yYO-XA7aF3i72EpgrDeyUp gically speaking, approximately 97 percent of tropical cyclones that form in the North Atlantic develop between the dates of June 1 and November 30 b dates which delimit the modern-day Atlantic hurricane season. Though the beginning of the annual hurricane season has historically remained the same, the official end of the hurricane season has shifted from its initial date of October 31. Regardless, on average once every few years a tropical cyclone develops outside the limits of the season; as of January 2016 there have been 68 tropical cyclones in the off-season, with the most recent being Subtropical Storm Andrea in 2019. The first tropical cyclone of the 1938 Atlantic hurricane season, which formed on January 3, became the earliest forming tropical storm and hurricane after reanalysis concluded on the storm in December 2012. No Hurricane Able in 1951 was initially thought to be the earliest forming major hurricane b a tropical cyclone with winds exceeding 115 mph (185 km/h)[nb 1] b however following post-storm analysis it was determined that Able only reached Category 1 strength which made Hurricane Alma of 1966 the new record holder; as it became a major hurricane on June 8. Though it developed within the bounds of the Atlantic hurricane season, Hurricane Audrey in 1957 became the earliest developing Category 4 hurricane on record after it reached the intensity on June 27. However, reanalysis from 1956 to 1960 by NOAA downgraded Audrey to a Category 3, making Hurricane Dennis of 2005 the earliest Category 4 on record on July 8, 2005. The earliest-forming Category 5 hurricane, Emily, reached the highest intensity on the SaffirbSimpson hurricane wind scale on July 17, 2005. Though the official end of the Atlantic hurricane season occurs on November 30, the dates of October 31 and November 15 have also historically marked the official end date for the hurricane season. December, the only month of the year after the hurricane season, has featured the cyclogenesis of fourteen tropical cyclones. Tropical Storm Zeta in 2005 was the latest tropical cyclone to attain tropical storm intensity as it did so on December 30. However, the second Hurricane Alice in 1954 was the latest forming tropical cyclone to attain hurricane intensity. Both Zeta and Alice were the only two storms to exist in two calendar years b the former from 1954 to 1955 and the latter from 2005 to 2006. No storms have been recorded to exceed Category 1 hurricane intensity in December. In 1999, Hurricane Lenny reached Category 4 intensity on November 17 as it took an unprecedented west to east track across the Caribbean; its intensity made it the latest developing Category 4 hurricane, though this was well within the bounds of the hurricane season. Hurricane Hattie (October 27 b November 1, 1961) was initially thought to have been the latest forming Category 5 hurricane ever documented, though reanalysis indicated that a devastating hurricane in 1932 reached such an intensity at a later date. Consequently, this made the hurricane the latest developing tropical cyclone to reach all four SaffirbSimpson hurricane wind scale classificati ------------------------------ Date: Sun, 24 May 2020 11:26:32 -0400 From: "Learn Photo Editing" Subject: In this 52-minute video tutorial we will use advanced color grading techniques to create In this 52-minute video tutorial we will use advanced color grading techniques to create http://smartclean.guru/tTTGDa6MnK6tKlbqk95ZEkjAMRx1Wqc58RwIw1yt4roXCk-Q http://smartclean.guru/VStf90fxpYeqCQIuJ6dO-igdaxIK2HF6wtOSyvHIpEByV5kb ersity was one of only eight United Kingdom universities to hold a parliamentary seat in the House of Commons at Westminster until such representation was abolished in 1950. The university was also represented in the Parliament of Northern Ireland from 1920 to 1968, when graduates elected four members. Contemporary university life On 20 June 2006, the university announced a B#259 million investment programme focusing on facilities, recruitment and research. One of the outcomes of this investment has been a new university library; the McClay library was designed by Boston-based architects Sheply, Bulfinch, Richardson & Abbott, working in association with Belfast architects, Robinson Patterson Partnership, and opened in July 2009. The building has been named in honour of Sir Allen McClay, a major benefactor of Queen's University and of the Library. In June 2010, the university announced the launch of a B#7.5m Ansin international research hub with Seagate Technologies. Queen's is one of the largest employers in Northern Ireland, with a total workforce of 3,903, of whom 2,414 were members of academic, academic-related and research staff and 1,489 were administrative employees. In addition to the main campus on the southern fringes of Belfast city centre, the university has two associated university colleges, St Mary's and Stranmillis located in the west and south-west of the city respectively. These colleges offer teacher training for those who wish to pursue teaching careers and a range of degree courses, all of which are centred around a liberal arts core. While the university refers to its main site as a campus, the university's buildings are in fact spread over a number of public streets in South Belfast, primarily, University Road, University Square, University Street, Malone Road and Stranmillis Road, with other departments located further afield such as in Titanic Quar ------------------------------ End of alt.music.moxy-fruvous digest V14 #4235 **********************************************