[226195] in SIPB-AFS-requests
Breaking News: Refinance Rates Just Dropped!
daemon@ATHENA.MIT.EDU (Nigel, FHA Rate Guide)
Fri Jan 31 10:21:57 2025
From 89230-181141-333679-19357-sipb+2Dafsreq+2Dmtg=charon.mit.edu@mail.memobrain.sa.com Fri Jan 31 15:21:56 2025
Return-Path: <89230-181141-333679-19357-sipb+2Dafsreq+2Dmtg=charon.mit.edu@mail.memobrain.sa.com>
Delivered-To: sipb-afsreq-mtg@charon.mit.edu
Received: (qmail 18741 invoked from network); 31 Jan 2025 15:21:56 -0000
Received: from unknown (HELO tucson.memobrain.sa.com) (160.191.81.20)
by charon.mit.edu with SMTP; 31 Jan 2025 15:21:56 -0000
DKIM-Signature: v=1; a=rsa-sha1; c=relaxed/relaxed; s=k1; d=memobrain.sa.com;
h=Mime-Version:Content-Type:Date:From:Reply-To:Subject:To:Message-ID; i=NigelFHARateGuide@memobrain.sa.com;
bh=jtN1vP6As7ziXSA8nPSS5QS34wQ=;
b=e3brc03AmQqle9x4d86o9DRJty7VX76Yng3GKl4F0RFAX++04Ilfxipwo9cj2yW9LxIqSiqkoy6y
oHe+S6Bv8M1XovFoI5AvOj2x7ablprWusqYyTxJ6+SK8QlkX1JIm3ukXWLOjhawgLaa4yMzDouAf
lZ09mjEbc8jauLdW7cHBn3OP0tUpEq++06NvQFobyEjwLY5LKHOOrQWvpOi7EF5qZUmoT2ff9sE6
KJ7UrjxPTk8Wt1lub93mlG6yXZ65i99KW3BCfwdEWgAgS/U7gkn0HBiJMTBg65dplZeY4hhlSlyS
37X2ctTVnXudfx28720RKSH4rzPmZ0Atc6O0aQ==
DomainKey-Signature: a=rsa-sha1; c=nofws; q=dns; s=k1; d=memobrain.sa.com;
b=CgKOGfYBh3ic0yRdzGCsJqkMi1FX+rAcEXh/WMhqCh/ajqJ0evzD0N1scNrIzcvjonS8vby8odwr
TvfLcKIacQ6iN+fdT+/YMFzHB1RhQRO3xOjkE1EN19rVp2P5Mnz7eY+Q/Z8SvmrQt/BDb22vrops
Lz26OadBm/Xyyau6ZtA436gX+3OaKmfnjiif2cPgbN+dTHlEI2qxOeWyywkCUcN/Y69WUNOMbyo8
A+VtxXYw7KQ+XdNyaZQnsCMgcWbfgl09m0ZoJ27lRpX/RxLty6EhOZSviDYef4TFSDnj5Yu/mxNj
+JM1DNZfu5AE3gxMPxW2206suSemP3BwxnXdIw==;
Mime-Version: 1.0
Content-Type: multipart/alternative; boundary="ef3d65720cbb7563ffe190d56f2a50aa_2c395_5176f"
Date: Fri, 31 Jan 2025 16:21:17 +0100
From: "Nigel, FHA Rate Guide" <NigelFHARateGuide@memobrain.sa.com>
Reply-To: "FHA Rate Guide" <FHARateGuide@memobrain.sa.com>
Subject: Breaking News: Refinance Rates Just Dropped!
To: <sipb-afsreq-mtg@charon.mit.edu>
Message-ID: <dbpfr1kn4lwh0poh-k8zaqsav0zxk651b-2c395-5176f@memobrain.sa.com>
--ef3d65720cbb7563ffe190d56f2a50aa_2c395_5176f
Content-Type: text/plain; charset=UTF-8
Content-Transfer-Encoding: 8bit
Breaking News: Refinance Rates Just Dropped!
Don't Miss Out: Lower Rates Are Here!
Interest rates have just dropped, making now the perfect time to refinance your home.
This is your chance to lock in a lower monthly payment and save big over the life of your loan.
But don't wait— these rates won't last forever!
Take action today and secure your financial future with a cash-out refinance or lower rate.
The sooner you act, the more you save!
http://memobrain.sa.com/9k5UfjQzbonCftbwfPskmHOowrt0JwDbWYMnFvFYhfYSRvoDBQ
osphere is the lowest layer of Earth's atmosphere. It extends from Earth's surface to an average height of about 12 km (7.5 mi; 39,000 ft), although this altitude varies from about 9 km (5.6 mi; 30,000 ft) at the geographic poles to 17 km (11 mi; 56,000 ft) at the Equator, with some variation due to weather. The troposphere is bounded above by the tropopause, a boundary marked in most places by a temperature inversion (i.e. a layer of relatively warm air above a colder one), and in others by a zone that is isothermal with height.
Although variations do occur, the temperature usually declines with increasing altitude in the troposphere because the troposphere is mostly heated through energy transfer from the surface. Thus, the lowest part of the troposphere (i.e. Earth's surface) is typically the warmest section of the troposphere. This promotes vertical mixing (hence, the origin of its name in the Greek word ??????, tropos, meaning "turn"). The troposphere contains roughly 80% of the mass of Earth's atmosphere. The troposphere is denser than all its overlying layers because a larger atmospheric weight sits on top of the troposphere and causes it to be most severely compressed. Fifty percent of the total mass of the atmosphere is located in the lower 5.6 km (3.5 mi; 18,000 ft) of the troposphere.
Nearly all atmospheric water vapor or moisture is found in the troposphere, so it is the layer where most of Earth's weather takes place. It has basically all the weather-associated cloud genus types generated by active wind circulation, although very tall cumulonimbus thunder clouds can penetrate the tropopause from below and rise into the lower part of the stratosphere. Most conventional aviation activity takes place in the troposph
If you wish to no longer receive emails from FHARateGuide, please unsubscribe here. Or, you can submit a written request at 12121 Wilshire Blvd, Suite 810 Los Angeles, CA 90025.
http://memobrain.sa.com/k4wJ6QLyVzzGk-W3qx6qlSZZV9uKzD8akBV2VWF1yAaFYFc0wA
--ef3d65720cbb7563ffe190d56f2a50aa_2c395_5176f
Content-Type: text/html; charset=UTF-8
Content-Transfer-Encoding: 8bit
<html>
<head>
<title>Newsletter</title>
</head>
<body><a href="http://memobrain.sa.com/RINRatAIIqQCq6i2-lDhEnRcaru7paAT_pTkrT0M3naJv8g2Xw"><img src="http://memobrain.sa.com/53305bd010b2c0140f.jpg" /><img src="http://www.memobrain.sa.com/A8twUhQ9SktnBiqqjSx0zUjV2wBxew5wcHgtFxRnybNOJ4NC7g" /></a>
<div style="width:600px;font-family:Helvetica,Arial,sans-serif;line-height:28px;font-size:18px;padding:20px;text-align:left;">Don't Miss Out: Lower Rates Are Here!<br />
<br />
Interest rates have just dropped, making now the perfect time to refinance your home.<br />
<br />
This is your chance to lock in a lower monthly payment and save big over the life of your loan.<br />
<br />
But don't wait— these rates won't last forever!<br />
<br />
<a href="http://memobrain.sa.com/9k5UfjQzbonCftbwfPskmHOowrt0JwDbWYMnFvFYhfYSRvoDBQ" http:="" microsoft.com="" rel="sponsored" target="blank"><b>Take action today</b></a> and secure your financial future with a cash-out refinance or lower rate.<br />
<br />
The sooner you act, the more <a href="http://memobrain.sa.com/9k5UfjQzbonCftbwfPskmHOowrt0JwDbWYMnFvFYhfYSRvoDBQ" http:="" microsoft.com="" rel="sponsored" target="blank"><b>you save!</b></a><br />
<br />
<div style="color:#FFFFFF;line-height:8px;">osphere is the lowest layer of Earth's atmosphere. It extends from Earth's surface to an average height of about 12 km (7.5 mi; 39,000 ft), although this altitude varies from about 9 km (5.6 mi; 30,000 ft) at the geographic poles to 17 km (11 mi; 56,000 ft) at the Equator, with some variation due to weather. The troposphere is bounded above by the tropopause, a boundary marked in most places by a temperature inversion (i.e. a layer of relatively warm air above a colder one), and in others by a zone that is isothermal with height. Although variations do occur, the temperature usually declines with increasing altitude in the troposphere because the troposphere is mostly heated through energy transfer from the surface. Thus, the lowest part of the troposphere (i.e. Earth's surface) is typically the warmest section of the troposphere. This promotes vertical mixing (hence, the origin of its name in the Greek word τρ?πος, tropos, meaning "turn"). The troposphere contains roughly 80% of the mass of Earth's atmosphere. The troposphere is denser than all its overlying layers because a larger atmospheric weight sits on top of the troposphere and causes it to be most severely compressed. Fifty percent of the total mass of the atmosphere is located in the lower 5.6 km (3.5 mi; 18,000 ft) of the troposphere. Nearly all atmospheric water vapor or moisture is found in the troposphere, so it is the layer where most of Earth's weather takes place. It has basically all the weather-associated cloud genus types generated by active wind circulation, although very tall cumulonimbus thunder clouds can penetrate the tropopause from below and rise into the lower part of the stratosphere. Most conventional aviation activity takes place in the troposph</div>
<br />
<br />
<br />
<div style="font-size:12px;">If you wish to no longer receive emails from FHARateGuide, please <a href="http://memobrain.sa.com/adZ9uh0kXogHb8OKSXfxtehASm-P7qtoRZMzhEBhXKT64cL5nQ" http:="" microsoft.com="" target="blank">unsubscribe</a> here. Or, you can submit a written request at 12121 Wilshire Blvd, Suite 810 Los Angeles, CA 90025.</div>
<br />
<br />
<br />
</div>
</body>
</html>
--ef3d65720cbb7563ffe190d56f2a50aa_2c395_5176f--
