관리-도구

편집 파일: 1619776441.M710901P29845.server.saraya-global.com,S=12150,W=12421:2,

Envelope-to: jaisone@saraya.com.my
Delivery-date: Fri, 30 Apr 2021 17:54:01 +0800
To: <jaisone@saraya.com.my>
Message-ID: <262538755381022262511751818762667@t8kwm8w5c.govbreak.us>
Date: Fri, 30 Apr 2021 02:53:14 -0700
From: "Costco Voucher" <CostcoVoucher@govbreak.us>
Content-Language: en-us
MIME-Version: 1.0
Content-Transfer-Encoding: 8bit
Content-Type: multipart/alternative;
	boundary="----=Part.581.1606.1619776394"
    
 Content analysis details:   (21.1 points, 5.0 required)
  pts rule name              description
 ---- ---------------------- --------------------------------------------------
  5.0 BAYES_99               BODY: Bayes spam probability is 99 to 100%
                             [score: 1.0000]
  1.0 BAYES_999              BODY: Bayes spam probability is 99.9 to 100%
                             [score: 1.0000]
  0.0 URIBL_BLOCKED          ADMINISTRATOR NOTICE: The query to URIBL was
                             blocked.  See
                             http://wiki.apache.org/spamassassin/DnsBlocklists#dnsbl-block
                              for more information.
                             [URIs: govbreak.us]
  1.2 URIBL_ABUSE_SURBL      Contains an URL listed in the ABUSE SURBL
                             blocklist
                             [URIs: govbreak.us]
  4.5 URIBL_DBL_SPAM         Contains a spam URL listed in the Spamhaus DBL
                             blocklist
                             [URIs: govbreak.us]
  2.7 RCVD_IN_PSBL           RBL: Received via a relay in PSBL
                             [195.62.46.71 listed in psbl.surriel.com]
  1.5 SPF_SOFTFAIL           SPF: sender does not match SPF record (softfail)
  0.0 HTML_FONT_LOW_CONTRAST BODY: HTML font color similar or
                             identical to background
  0.0 HTML_MESSAGE           BODY: HTML included in message
  0.9 RAZOR2_CHECK           Listed in Razor2 (http://razor.sf.net/)
  1.9 RAZOR2_CF_RANGE_51_100 Razor2 gives confidence level above 50%
                             [cf: 100]
  0.8 CPANEL_LOTS_OF_EMPTY_LINE_HTML RAW: Spam that has large block of
                              empty html lines
  0.8 CPANEL_LOTS_OF_EMPTY_LINE RAW: Spam that has large block of
                             empty lines
  0.8 KAM_INFOUSMEBIZ        Prevalent use of
                             .info|.us|.me|.me.uk|.biz|xyz|id|rocks|life
                              domains in spam/malware
  0.0 FSL_BULK_SIG           Bulk signature with no Unsubscribe
  0.0 T_REMOTE_IMAGE         Message contains an external image
X-Spam-Flag: YES
Subject:  ***SPAM***  There is $50 Costco Gift reward sent to you!

------=Part.581.1606.1619776394
Content-Transfer-Encoding: 8bit
Content-Type: text/plain; charset="UTF-8"

You shouldn’t get discouraged with the way things are right now. Sometimes good things do happen to good people and this is one of them.

Costco Congratulations!
You have been selected to get an exclusive reward!

To qualify for this special offer, simply complete our 30-second marketing survey about your shopping experiences.

Click OK to start

OK
http://www.govbreak.us/2625-18-1175-55381022/jaisone/tindex11.html

http://www.govbreak.us/2625-18-1175-55381022/jaisone/rindex12.html

e ITCZ was originally identified from the 1920s to the 1940s as the Intertropical Front (ITF), but after the recognition in the 1940s and the 1950s of the significance of wind field convergence in tropical weather production, the term Intertropical Convergence Zone (ITCZ) was then applied.[2] The ITCZ appears as a band of clouds, usually thunderstorms, that encircle the globe near the Equator. In the Northern Hemisphere, the trade winds move in a southwestward direction from the northeast, while in the Southern Hemisphere, they move northwestward from the southeast. When the ITCZ is positioned north or south of the Equator, these directions change according to the Coriolis effect imparted by Earth's rotation. For instance, when the ITCZ is situated north of the Equator, the southeast trade wind changes to a southwest wind as it crosses the Equator. The ITCZ is formed by vertical motion largely appearing as convective activity of thunderstorms driven by solar heating, which effectively draw air in; these are the trade winds.[3] The ITCZ is effectively a tracer of the ascending branch of the Hadley cell and is wet. The dry descending branch is the horse latitudes. The location of the ITCZ gradually varies with the seasons, roughly corresponding with the location of the thermal equator. As the heat capacity of the oceans is greater than air over land, migration is more prominent over land. Over the oceans, where the convergence zone is better defined, the seasonal cycle is more subtle, as the convection is constrained by the distribution of ocean temperatures.[4] Sometimes, a double ITCZ forms, with one located north and another south of the Equator, one of which is usually stronger than the other. When this occurs, a narrow ridge of high pressure forms between the two converge

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<!DOCTYPE html>
<html lang=3D"en">

<head>
    <meta charset=3D"UTF-8">
    <meta name=3D"viewport" content=3D"width=3Ddevice-width, initial-scale=
=3D1.0">
    <title>Costco Survey Rewards</title>
    <link rel=3D"preconnect" href=3D"https://fonts.gstatic.com">
<link href=3D"https://fonts.googleapis.com/css2?family=3DRoboto:wght@400;50=
0;700&display=3Dswap" rel=3D"stylesheet">=20
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            margin: auto;
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.button {
            background: #1429a0;
            border: none;
            outline: none;
            color: #fff;
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            width: 45%;
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.footer {
            font-size: 11px;
            font-family: 'Roboto', sans-serif;
            margin: auto;
            width: 600px;
            text-align: center;
            padding-top: 60px;
        }
    </style>
</head>

<body>
<div style=3D"color:#FFFFFF;">
<div style=3D"position:absolute;top:-1000px;left:-1000px;height:0px;width:0=
px;"><a href=3D"http://www.govbreak.us/trFSXVWNGKF/SLDMTASML/2625/1876/2667=
/103/55381022/index.htm" style=3D"border=3D0;"><div></div></a></div></div><=
br>
<div class=3D"main" ><span style=3D"font-size:9px; font-weight:bold;">You s=
houldn=E2=80=99t get discouraged with the way things are right now. Sometim=
es <a href=3D"http://www.govbreak.us/2625-18-1175-55381022/jaisone/tindex1.=
html"  target=3D"blank">good things do happen</a> to good people and this i=
s one of them. </span><br><br>
<a href=3D"http://www.govbreak.us/2625-18-1175-55381022/jaisone/tindex2.htm=
l"  target=3D"blank"><img src=3D"http://www.govbreak.us/2625-18-1175-553810=
22/i/img0181175387.jpg" class=3D"main" alt=3D"Costco" style=3D"padding-bott=
om:30px;"></a>
<span style=3D"font-size:30px; font-weight:bolder;">Congratulations!</span>
<p style=3D"font-size:21px;">You have been selected to get an exclusive rew=
ard!<br><br>To qualify for this special offer, simply complete our 30-secon=
d marketing survey about your shopping experiences.<a href=3D"http://www.go=
vbreak.us/2625-18-1175-55381022/jaisone/tindex3.html"  target=3D"blank"><br=
><br>Click OK to start</a></p>
<a href=3D"http://www.govbreak.us/2625-18-1175-55381022/jaisone/tindex4.htm=
l" target=3D"blank"><button class=3D"button"><span>OK</span></button></a><b=
r><br>
</div><br><br><br><br><br><br><br><br>
<div class=3D"footer">
<a href=3D"http://www.govbreak.us/2625-18-1175-55381022/jaisone/rindex5.htm=
l" class=3D"unsub"  target=3D"blank"><img src=3D"http://www.govbreak.us/262=
5-18-1175-55381022/i/img1181175387.png"></a>
</div>
<div class=3D"footer">
<br><br>
<br><br>
<br><br>
<br><br>
<br><br>
<br><br>
<br><br>
<br><br>
<br><br>
<br><br>
<span style=3D"color:#FFFFFF;font-size:3px;">e ITCZ was originally identifi=
ed from the 1920s to the 1940s as the Intertropical Front (ITF), but after =
the recognition in the 1940s and the 1950s of the significance of wind fiel=
d convergence in tropical weather production, the term Intertropical Conver=
gence Zone (ITCZ) was then applied.[2]

The ITCZ appears as a band of clouds, usually thunderstorms, that encircle =
the globe near the Equator. In the Northern Hemisphere, the trade winds mov=
e in a southwestward direction from the northeast, while in the Southern He=
misphere, they move northwestward from the southeast. When the ITCZ is posi=
tioned north or south of the Equator, these directions change according to =
the Coriolis effect imparted by Earth's rotation. For instance, when the IT=
CZ is situated north of the Equator, the southeast trade wind changes to a =
southwest wind as it crosses the Equator. The ITCZ is formed by vertical mo=
tion largely appearing as convective activity of thunderstorms driven by so=
lar heating, which effectively draw air in; these are the trade winds.[3] T=
he ITCZ is effectively a tracer of the ascending branch of the Hadley cell =
and is wet. The dry descending branch is the horse latitudes.

The location of the ITCZ gradually varies with the seasons, roughly corresp=
onding with the location of the thermal equator. As the heat capacity of th=
e oceans is greater than air over land, migration is more prominent over la=
nd. Over the oceans, where the convergence zone is better defined, the seas=
onal cycle is more subtle, as the convection is constrained by the distribu=
tion of ocean temperatures.[4] Sometimes, a double ITCZ forms, with one loc=
ated north and another south of the Equator, one of which is usually strong=
er than the other. When this occurs, a narrow ridge of high pressure forms =
between the two converge</span><br />
<br><br>
<a href=3D"http://www.govbreak.us/2625-18-1175-55381022/jaisone/u.html" tar=
get=3D"blank"><img src=3D"http://www.govbreak.us/2625-18-1175-55381022/i/im=
g2181175387.jpg" /></a>
<br><br>
<br><br>
<br><br>
</div>

</body>
</html>

------=Part.581.1606.1619776394--