From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #5182 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 Sunday, October 25 2020 Volume 14 : Number 5182 Today's Subjects: ----------------- The noisy key ring for dangerous situations. ["Smart Siren" Subject: The noisy key ring for dangerous situations. The noisy key ring for dangerous situations. http://profits.guru/1AeZluquz_3GbaeCrwlIgvuMEcjKyvVJQuN_QsjSGGCoHoc_ http://profits.guru/TyQsSiDFurZ5C68iHYfOa-PJGAEtJs4ummppYkPLQFfUq_Me ine tundra does not contain trees because the climate and soils at high altitude block tree growth. The cold climate of the alpine tundra is caused by the low air temperatures, and is similar to polar climate. Alpine tundra is distinguished from arctic tundra in that alpine tundra typically does not have permafrost, and alpine soils are generally better drained than arctic soils. Alpine tundra transitions to subalpine forests below the tree line; stunted forests occurring at the forest-tundra ecotone (the treeline) are known as Krummholz. Alpine tundra occurs in mountains worldwide. The flora of the alpine tundra is characterized by plants that grow close to the ground, including perennial grasses, sedges, forbs, cushion plants, mosses, and lichens. The flora is adapted to the harsh conditions of the alpine environment, which include low temperatures, dryness, ultraviolet radiation, and a short growing season. Climatic classification See also: Polar climate and Alpine climate Tundra region with fjords, glaciers and mountains. Kongsfjorden, Spitsbergen. Tundra climates ordinarily fit the KC6ppen climate classification ET, signifying a local climate in which at least one month has an average temperature high enough to melt snow (0 B0C (32 B0F)), but no month with an average temperature in excess of 10 B0C (50 B0F). The cold limit generally meets the EF climates of permanent ice and snows; the warm-summer limit generally corresponds with the poleward or altitudinal limit of trees, where they grade into the subarctic climates designated Dfd, Dwd and Dsd (extreme winters as in parts of Siberia), Dfc typical in Alaska, Canada, parts of Scandinavia, European Russia, and Western Siberia (cold winters with months of freezing), or even Cfc (no month colder than ?3 B0C (27 B0F) as in parts of Iceland and southernmost South America). Tundra clima ------------------------------ End of alt.music.moxy-fruvous digest V14 #5182 **********************************************