From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #14779 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 Friday, September 27 2024 Volume 14 : Number 14779 Today's Subjects: ----------------- Leave your feedback and you could WIN! ["We value your feedback" Subject: Leave your feedback and you could WIN! Leave your feedback and you could WIN! http://powerpatriots.sa.com/AeaqlIfZOM9G7fhVZ7FiIjFCe86hoFhULrkSg9_q13xJ4Z0nZA http://powerpatriots.sa.com/yRKAOF1-d6ly_EpYEQA0RyJPr-_kSZBD3pFpeEepxWPXMaeZxQ ervations reinforce the evidence of warming. The upper atmosphere is cooling, because greenhouse gases are trapping heat near the Earth's surface, and so less heat is radiating into space. Warming reduces average snow cover and forces the retreat of glaciers. At the same time, warming also causes greater evaporation from the oceans, leading to more atmospheric humidity, more and heavier precipitation. Plants are flowering earlier in spring, and thousands of animal species have been permanently moving to cooler areas. Differences by region Different regions of the world warm at different rates. The pattern is independent of where greenhouse gases are emitted, because the gases persist long enough to diffuse across the planet. Since the pre-industrial period, the average surface temperature over land regions has increased almost twice as fast as the global average surface temperature. This is because oceans lose more heat by evaporation and oceans can store a lot of heat. The thermal energy in the global climate system has grown with only brief pauses since at least 1970, and over 90% of this extra energy has been stored in the ocean. The rest has heated the atmosphere, melted ice, and warmed the continents. The Northern Hemisphere and the North Pole have warmed much faster than the South Pole and Southern Hemisphere. The Northern Hemisphere not only has much more land, but also more seasonal snow cover and sea ice. As these surfaces flip from reflecting a lot of light to being dark after the ice has melted, they start absorbing more heat. Local black carbon deposits on snow and ice also contribute to Arctic warming. Arctic surface temperatures are increasing between three and four times faster than in the rest of the world. Melting of ice sheets near the poles weakens both the Atlantic and the Antarctic limb of thermohaline circulation, which further changes the distribution of heat and precipitation around the globe. Future global temperatures CMIP6 multi-model projections of global surface temperature changes for the year 2090 relative to the 1850b1900 average. The current trajectory for warming by the end of the century is roughly halfway between these two extremes. The World Meteorological Organization estimates a 66% chance of global temperatures exceeding 1.5 B0C warming from the preindustrial baseline for at least one year betwe ------------------------------ End of alt.music.moxy-fruvous digest V14 #14779 ***********************************************