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From: "Keto Recipes" <ketodiet@biospirkill.us>
To: <christian.gabriel@shortnote.de>
Subject: *****SPAM***** Get this brand new simply tasty ketogenic cookbook
Date: Wed, 19 Dec 2018 11:15:56 -0500
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Content preview: This email must be viewed in HTML mode. There's only a few
left and I wanted to check and see if you wanted this for free but... Want
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Date: Wed, 19 Dec 2018 11:15:56 -0500
From: "Keto Recipes" <ketodiet@biospirkill.us>
Reply-To: "Fat-Shredding Keto Diet" <ketodiet@biospirkill.us>
Subject: Get this brand new simply tasty ketogenic cookbook
To: <christian.gabriel@shortnote.de>
Message-ID: <ormyx5ljrojeusmz-efguhe6uppz9cfcb-f0c46eeb@biospirkill.us>
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<body><a href="http://biospirkill.us/aDhxTEMhEign2vujNGBT_RWGn15kNMk-WbTUIWJX_G85O1wT"><img border="0" src="http://biospirkill.us/bptgfpUHGtkjM_3ik1cXW6AMP7RAVPlFI6lYvb8h6tdDQvop" /> </a>
<p style=" font-size: 15px; font-family: arial; "> </p>
<p> </p>
<div style=" font-size: 15px; font-family: arial; ">There's only a few left and I wanted to check and see if you wanted this for free but...<br />
<br />
Want to know the secret to pretty much every diet out there? Here it is...<br />
<br />
Most of the time, your body burns carbs for fuel. Any excess carbs you<br />
don't burn are stored as fat. However...<br />
<br />
By limiting your carb and protein intake, you can actually FORCE your<br />
body into a state of "ketosis." In this state, your body "learns"<br />
how to burn fat for fuel. And...<br />
<br />
Get this...<br />
<br />
Almost every diet out there relies on ketosis for fat loss! So...<br />
<br />
How exactly do you get into ketosis? Simple! All you have to do is eat the<br />
keto recipes in this brand new <a href="http://biospirkill.us/8XR9FY2h3jIHrYyEk8tIpp24LouiUIbw7hrIibU5-JyImLZZ" style="color:#0000FF;"><b>FREE cookbook called The Simply<br />
Tasty Ketogenic Cookbook. </b></a>
<p><a href="http://biospirkill.us/8XR9FY2h3jIHrYyEk8tIpp24LouiUIbw7hrIibU5-JyImLZZ"><img src="http://biospirkill.us/1a2a900ee0ff6b918a.jpg" /> </a></p>
<br />
This book is jam-packed with 150 delicious fat-shredding ketogenic recipes<br />
that will help you burn fat like crazy. Even stubborn belly and thigh fat won't<br />
stand a chance because your body will have NO CHOICE but to burn that fat for fuel!<br />
<br />
<b>=><a href="http://biospirkill.us/8XR9FY2h3jIHrYyEk8tIpp24LouiUIbw7hrIibU5-JyImLZZ" style="color:#0000FF;"> You can get your free The Simply Tasty Ketogenic Cookbook</a></b><br />
<br />
But please hurry since there were only 300 copies printed when they first started<br />
(this print run) they'll likely be gone. Once those books have been claimed,<br />
it could take weeks to get more in stock.<br />
<br />
-Elvira Horton<br />
</div>
<p> </p>
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<td colspan="2" style="background-color:#ffffff"><span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif; font-size:4px">much as 31%, but Debbie regained its strength after each of two seeding forays. In an earlier episode in 1947, disaster struck when a hurricane east of Jacksonville, Florida promptly changed its course after being seeded, and smashed into Savannah, Georgia. Because there was so much uncertainty about the behavior of these storms, the federal government would not approve seeding operations unless the hurricane had a less than 10% chance of making landfall within 48 hours, greatly reducing the number of possible test storms. The project was dropped after it was discovered that eyewall replacement cycles occur naturally in strong hurricanes, casting doubt on the result of the earlier attempts. Today, it is known that silver iodide seeding is not likely to have an effect because the amount of supercooled water in the rainbands of a tropical cyclone is too low. </span><br />
<br />
<span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif; font-size:4px">In the 1960s and 1970s, the United States government attempted to weaken hurricanes through Project Stormfury by seeding selected storms with silver iodide. It was thought that the seeding would cause supercooled water in the outer rainbands to freeze, causing the inner eyewall to collapse and thus reducing the winds. The winds of Hurricane Debbie—a hurricane seeded in Project Stormfury—dropped as </span><br />
<br />
<span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif; font-size:4px">days. Even after a tropical cyclone is said to be extratropical or dissipated, it can still have tropical storm force (or occasionally hurricane/typhoon force) winds and drop several inches of rainfall. In the Pacific Ocean and Atlantic Ocean, such tropical-derived cyclones of higher latitudes can be violent and may occasionally remain at hurricane or typhoon-force wind speeds when they reach the west coast of North America. These phenomena can also affect Europe, where they are known as European windstorms; Hurricane Iris's extratropical remnants are an example of such a windstorm from 1995. A cyclone can also merge with another area of low pressure, becoming a larger area of low pressure. This can strengthen the resultant system, although it may no longer be a tropical cyclone. Studies in the 2000s have given rise to the hypothesis that large amounts of dust reduce the strength of tropical cyclones. Artificial dissipation </span><br />
<br />
<span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif; font-size:4px">A tropical cyclone can dissipate when it moves over waters significantly below 26.5 °C (79.7 °F). This will cause the storm to lose its tropical characteristics, such as a warm core with thunderstorms near the center, and become a remnant low-pressure area. These remnant systems may persist for up to several days before losing their identity. This dissipation mechanism is most common in the eastern North Pacific. Weakening or dissipation can occur if it experiences vertical wind shear, causing the convection and heat engine to move away from the center; this normally ceases development of a tropical cyclone. In addition, its interaction with the main belt of the Westerlies, by means of merging with a nearby frontal zone, can cause tropical cyclones to evolve into extratropical cyclones. This transition can take 1–3 </span><br />
<br />
<span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif; font-size:4px">A tropical cyclone can cease to have tropical characteristics in several different ways. One such way is if it moves over land, thus depriving it of the warm water it needs to power itself, quickly losing strength. Most strong storms lose their strength very rapidly after landfall and become disorganized areas of low pressure within a day or two, or evolve into extratropical cyclones. There is a chance a tropical cyclone could regenerate if it managed to get back over open warm water, such as with Hurricane Ivan. If it remains over mountains for even a short time, weakening will accelerate. Many storm fatalities occur in mountainous terrain, when diminishing cyclones unleash their moisture as torrential rainfall. This rainfall may lead to deadly floods and mudslides, as was the case with Hurricane Mitch around Honduras in October 1998. Without warm surface water, the storm cannot survive. </span><br />
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