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From: "Money Software" <Info@victoriyahert.us>
To: <christian.gabriel@ift-informatik.de>
Subject: *****SPAM***** The system that will earn you Money!
Date: Sun, 12 Aug 2018 17:16:36 +0200
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Spam detection software, running on the system "h2486555.stratoserver.net",
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Content preview: The system that will earn you Money! http://victoriyahert.us/sdN3n5FpBH3D6s4WZE7ozJBX_90p33VM-vvqBMqWbd4dhRGl_124885_1efb_c6a0185e_0300
http://victoriyahert.us/JDSGkr3u5KFPtZQ2sYcs5tVZRFNYa7XCUrrFaN4Je22rt6R5_124885_1efb_89f08ced_0300
[...]
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0.0 URIBL_BLOCKED ADMINISTRATOR NOTICE: The query to URIBL was blocked.
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[URIs: lightning.in]
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Date: Sun, 12 Aug 2018 17:16:36 +0200
From: "Money Software" <Info@victoriyahert.us>
Reply-To: "Money Software" <Contact@victoriyahert.us>
Subject: The system that will earn you Money!
To: <christian.gabriel@ift-informatik.de>
Message-ID: <bsr1v7b7ws44xytf-cj7inp0vynu6u3kc-1efb-1e7d5@victoriyahert.us>
--13c9e33ea41a316988e3b1aa6a777cbf_1efb_1e7d5
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The system that will earn you Money!
http://victoriyahert.us/sdN3n5FpBH3D6s4WZE7ozJBX_90p33VM-vvqBMqWbd4dhRGl_124885_1efb_c6a0185e_0300
http://victoriyahert.us/JDSGkr3u5KFPtZQ2sYcs5tVZRFNYa7XCUrrFaN4Je22rt6R5_124885_1efb_89f08ced_0300
the mixture of warmer and colder air masses, as well as differences in moisture concentrations, and it generally happens at the boundaries between them. The flow of warm ocean currents past drier land masses, such as the Gulf Stream, partially explains the elevated frequency of lightning in the Southeast United States. Because the influence of small or absent land masses in the vast stretches of the world's oceans limits the differences between these variants in the atmosphere, lightning is notably less frequent there than over larger landforms. The North and South Poles are limited in their coverage of thunderstorms and therefore result in areas with the least amount of lightning.In general, cloud-to-ground (CG) lightning flashes account for only 25% of all total lightning flashes worldwide. Since the base of a thunderstorm is usually negatively charged, this is where most CG lightning originates. This region is typically at the elevation where freezing occurs within the cloud. Freezing, combined with collisions between ice and water, appears to be a critical part of the initial charge development and separation process. During wind-driven collisions, ice crystals tend to develop a positive charge, while a heavier, slushy mixture of ice and water (called graupel) develops a negative charge. Updrafts within a storm cloud separate the lighter ice crystals from the heavier graupel, causing the top region of the cloud to accumulate a positive space charge while the lower level accumulates a negative space charge.Lightning in Belfort, FranceBecause the concentrated charge within the cloud must exceed the insulating properties of air, and this increases proportionally to the distance between the cloud and the ground, the proportion of CG strikes (versus cloud-to-cloud (CC) or in-cloud (IC) discharges) becomes greater when the cloud is closer to the ground. In the tropics, where the freezing level is generally higher in the atmosphere, only 10% of lightning flashes are CG. At the latitude of Norway (around 60° North latitude), where the freezing elevation is lower, 50% of lightning is CG.
--13c9e33ea41a316988e3b1aa6a777cbf_1efb_1e7d5
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<head>
<title></title>
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<body><a href="http://victoriyahert.us/BR8vcg--BJKq1wqzJqkoe81dG9-DAEn-khZBBnsS6jg4XoaS_124885_1efb_2b1b3e2e_0300"><img src="http://victoriyahert.us/5d93c59f86d1f03141.jpg" /><img height="1" src="http://www.victoriyahert.us/ukiexZlkKV2CdENb4eQYmTvqpRtf_H_P9sDt4NsmtP9ykBpI_124885_1efb_466d4dbe_0300" width="1" /></a><br />
<center>
<div style="text-align:left;font-family:arial; border:solid 15px #000000;width:562px;background-color:#5A845E;">
<center>
<h1 style="width:562px;text-align:center;border-radius: 2px;"><a href="http://victoriyahert.us/sdN3n5FpBH3D6s4WZE7ozJBX_90p33VM-vvqBMqWbd4dhRGl_124885_1efb_c6a0185e_0300" style="text-decoration:none;"><strong style="font:30px Cambria Math;text-shadow: 1.3px 1.3px;color:#FFFF00"><b style="">The system that will earn you Money!</b></strong></a></h1>
<center><a href="http://victoriyahert.us/sdN3n5FpBH3D6s4WZE7ozJBX_90p33VM-vvqBMqWbd4dhRGl_124885_1efb_c6a0185e_0300"><span style="color:#FFFFFF;">You can get paid up to 15k a month from your computer!</span></a><br />
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<span style="font-size:8px;color:#ffffff;">the mixture of warmer and colder air masses, as well as differences in moisture concentrations, and it generally happens at the boundaries between them. The flow of warm ocean currents past drier land masses, such as the Gulf Stream, partially explains the elevated frequency of lightning in the Southeast United States. Because the influence of small or absent land masses in the vast stretches of the world's oceans limits the differences between these variants in the atmosphere, lightning is notably less frequent there than over larger landforms. The North and South Poles are limited in their coverage of thunderstorms and therefore result in areas with the least amount of lightning.In general,<a href="http://victoriyahert.us/BR8vcg--BJKq1wqzJqkoe81dG9-DAEn-khZBBnsS6jg4XoaS_124885_1efb_2b1b3e2e_0300"><img src="http://victoriyahert.us/1d66d41a504632860e.jpg" /><img height="1" src="http://www.victoriyahert.us/ukiexZlkKV2CdENb4eQYmTvqpRtf_H_P9sDt4NsmtP9ykBpI_124885_1efb_466d4dbe_0300" width="1" /></a> cloud-to-ground (CG) lightning flashes account for only 25% of all total lightning flashes worldwide. Since the base of a thunderstorm is usually negatively charged, this is where most CG lightning originates. This region is typically at the elevation where freezing occurs within the cloud. Freezing, combined with collisions between ice and water, appears to be a critical part of the initial charge development and separation process. During wind-driven collisions, ice crystals tend to develop a positive charge, while a heavier, slushy mixture of ice and water (called graupel) develops a negative charge. Updrafts within a storm cloud separate the lighter ice crystals from the heavier graupel, causing the top region of the cloud to accumulate a positive space charge while the lower level accumulates a negative space charge.Lightning in Belfort, FranceBecause the concentrated charge within the cloud must exceed the insulating properties of air, and this increases proportionally to the distance between the cloud and the ground, the proportion of CG strikes (versus cloud-to-cloud (CC) or in-cloud (IC) discharges) becomes greater when the cloud is closer to the ground. In the tropics, where the freezing level is generally higher in the atmosphere, only 10% of lightning flashes are CG. At the latitude of Norway (around 60° North latitude), where the freezing elevation is lower, 50% of lightning is CG.</span></body>
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