From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #10224 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 Saturday, December 3 2022 Volume 14 : Number 10224 Today's Subjects: ----------------- Prepping to Become ILLEGAL? ["Self Sufficiency" Subject: Prepping to Become ILLEGAL? Prepping to Become ILLEGAL? http://unitedairlines.ltd/7d7SvhKQYtAJKXUSnRBnxOpPErQ9kgix1sIErGD1FzrBxq4oqw http://unitedairlines.ltd/-9xvGo8BURc2cK4YYHtmN84LEh4zhdcZo4eQDF-KZbGkTkJ9Cg e water desalination plant became inoperable. Power lines were cut across the island. There were no deaths or significant injuries. Other islands in the nation had their water contaminated by saltwater, and 95 percent of the crops were destroyed by the storm surge. Coral reefs were also heavily damaged when the storm came nearby. As an extratropical cyclone, Zelda bought heavy rain and 110 km/h (70 mph) winds to Southeast Alaska. Heavy snow was reported in northern British Columbia, and lesser amounts inland British Columbia and southern Yukon. The United States Army engaged in clean up and repairing in the country. On December 6, the 834th Airlift Division sent six C-130s to Kwajalein with supplies. On the same day, President of the United States George H. W. Bush, through the Compact of Free Association, declared a major disaster in the Marshall Islands, allowing federal funding to be sent to the Arno, Aur, Kwajalein, Lae, Lib, Namu and Ujae islands. United States Senator Daniel Akaka visited Ebeye after the storm, and he criticized the response of the Federal Emergency Management Agency (FEMA), as the funding did not cover repairing of structures regarded as substandard. The Government of the Marshall Islands requested for aid via United Nations Disaster Relief Organization (UNDRO) on December 18. By December 19, 1,380 people were still living in temporary shelters. By March 26, 1992, abou ------------------------------ Date: Fri, 2 Dec 2022 16:43:09 +0100 From: "Motion Bright" Subject: Heavy Duty Industrial Light Heavy Duty Industrial Light http://sonuscompletez.shop/YJuKV6VgDK_z7W723MMdRVkD2Glyxsw4S-NHN9trQQC4oxGnnQ http://sonuscompletez.shop/lSY3fFini6o6sMGv8jl75bW8Y5xQjZ6LXXhoUCg5_7-4b5PRbg ighteen hours later. The JTWC reported that Zelda intensified into a typhoon at 12:00 UTC near the Marshall Islands, with winds of 65 kn (120 km/h; 75 mph), equivalent to a Category 1 on the SaffirbSimpson hurricane wind scale. At that time, the JMA kept it as a tropical storm with winds of 45 kn (85 km/h; 50 mph), with a pressure reading of 990 hectopascals (29 inHg). Around 06:00 UTC on November 30, the JMA estimated Zelda had reached its peak at 60 kn (110 km/h; 70 mph), with a barometric pressure of 975 hPa (28.8 inHg). Six hours later, the JTWC reported the storm had strengthened to maximum sustained winds of 80 kn (150 km/h; 90 mph), west of Enewetak. Later, a trough created by Typhoon Yuri caused the subtropical ridge to weaken, allowing Zelda to move northward. By December 1, the storm began to weaken and turned northeast. On December 2, the JMA reported the storm's winds had decreased to 50 kn (95 km/h; 60 mph). The JTWC reported the storm weakened below typhoon strength on 18:00 UTC of the same day, with winds of 60 kn (110 km/h; 70 mph). Upper-level winds and westerlies soon increased, and Zelda's central convection became sheared. The JMA downgraded Zelda to a tropical storm on December 3, and to a ------------------------------ Date: Fri, 2 Dec 2022 13:08:14 -0500 From: "Mistakes In Crisis" Subject: Why Civil War Is Possible and Terrifying... Why Civil War Is Possible and Terrifying... https://fortivacreaditcard.today/L652bjWJTFvD6tSLJ9Sd9X_LOmqdynCcslk4-mBtjYMhesqKig https://fortivacreaditcard.today/oXZZnyKWfBecvTRHW6t33xNM-L4nXnu1TyOBgCGUmnk17lQlHQ Warm sea surface temperatures are required in order for tropical cyclones to form and strengthen. The commonly-accepted minimum temperature range for this to occur is 26b27 B0C (79b81 B0F), however, multiple studies have proposed a lower minimum of 25.5 B0C (77.9 B0F). Higher sea surface temperatures result in faster intensification rates and sometimes even rapid intensification. High ocean heat content, also known as Tropical Cyclone Heat Potential, allows storms to achieve a higher intensity. Most tropical cyclones that experience rapid intensification are traversing regions of high ocean heat content rather than lower values. High ocean heat content values can help to offset the oceanic cooling caused by the passage of a tropical cyclone, limiting the effect this cooling has on the storm. Faster-moving systems are able to intensify to higher intensities with lower ocean heat content values. Slower-moving systems require higher values of ocean heat content to achieve the same intensity. The passage of a tropical cyclone over the ocean causes the upper layers of the ocean to cool substantially, a process known as upwelling, which can negatively influence subsequent cyclone development. This cooling is primarily caused by wind-driven mixing of cold water from deeper in the ocean with the warm surface waters. This effect results in a negative feedback process that can inhibit further development or lead to weakening. Additional cooling may come in the form of cold water from falling raindrops (this is because the atmosphere is cooler at higher altitudes). Cloud cover may also play a role in cooling the ocean, by shielding the ocean surface from direct sunlight before and slightly after the storm passage. All these effects can combine to produce a dramatic drop in sea surface temperature over a large area in just a few days. Conversely, the mixing of the sea can result in heat being inserted in deeper waters, with potential effects on global climate. Vertical wind shear negatively impacts tropical cyclone inte ------------------------------ End of alt.music.moxy-fruvous digest V14 #10224 ***********************************************