From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #11874 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 Monday, July 31 2023 Volume 14 : Number 11874 Today's Subjects: ----------------- Claim these incentives before they expire... ["EnergyBillCruncher Partner] ---------------------------------------------------------------------- Date: Mon, 31 Jul 2023 15:41:59 +0200 From: "EnergyBillCruncher Partner" Subject: Claim these incentives before they expire... Claim these incentives before they expire... http://unitedairlines.ltd/49-UPKynKNJ7MKe6kULQF2DKWHZeRgt2kPIO7EcmdL3zf2soog http://unitedairlines.ltd/kTwK8YL2y0_dl5sjqc58ySL62GGDwTlO0Xx-BaurGQ1JZQpjCg As part of the Hadley cell, surface air flows toward the equator while the flow aloft is towards the poles. A low-pressure area of calm, light variable winds near the equator is known as the doldrums, near-equatorial trough, intertropical front, or the Intertropical Convergence Zone. When located within a monsoon region, this zone of low pressure and wind convergence is also known as the monsoon trough. Around 30B0 in both hemispheres, air begins to descend toward the surface in subtropical high-pressure belts known as subtropical ridges. The subsident (sinking) air is relatively dry because as it descends, the temperature increases, but the moisture content remains constant, which lowers the relative humidity of the air mass. This warm, dry air is known as a superior air mass and normally resides above a maritime tropical (warm and moist) air mass. An increase of temperature with height is known as a temperature inversion. When it occurs within a trade wind regime, it is known as a trade wind inversion. The surface air that flows from these subtropical high-pressure belts toward the Equator is deflected toward the west in both hemispheres by the Coriolis effect. These winds blow predominantly from the northeast in the Northern Hemisphere and from the southeast in the Southern Hemisphere. Because winds are named for the direction from which the wind is blowing, these winds are called the northeasterly trade winds in the Northern Hemisphere and the southeasterly trade winds in the Southern Hemisphere. The trade winds of both hemispheres meet at the Doldrums. As they blow across tropical regions, air masses heat up over lower latitudes due to more direct sunlight. Those that develop over land (continental) are drier and hotter than those that develop over oceans (maritime), and travel northward on the western periphery of the subtropical ridge. Maritime tropical air masses are sometimes referred to as trade air masses. All tropical oceans except the northern Indian Ocean have extensive areas of trade winds ------------------------------ End of alt.music.moxy-fruvous digest V14 #11874 ***********************************************