[From nobody Sat Oct 10 08:22:39 2009 Return-Path: <owner-quaternary@CLIFFY.UCS.MUN.CA> Received: from mailrelay.williams.edu (EHLO mailrelay.williams.edu) ([137.165.4.207]) by miram5000a.williams.edu (MOS 3.10.4-GA FastPath queued) with ESMTP id AGV47961; Fri, 09 Oct 2009 14:14:54 -0400 (EDT) X-IronPort-Anti-Spam-Filtered: true X-IronPort-Anti-Spam-Result: AhADAEcaz0qGmegqmWdsb2JhbACBUlUuBJgtAQEBAQEICwoHE7A7AQmGVIhLgkyBYASBWA X-IronPort-AV: E=Sophos;i="4.44,533,1249272000"; d="scan'208,217";a="7520134" Received: from cliffy.ucs.mun.ca ([134.153.232.42]) by mailgate.williams.edu with ESMTP; 09 Oct 2009 14:14:52 -0400 Received: from cliffy.ucs.mun.ca (cliffy.ucs.mun.ca [134.153.232.42]) by cliffy.ucs.mun.ca (8.12.11.20060308/8.12.11) with ESMTP id n99HPqZu002575; Fri, 9 Oct 2009 15:36:32 -0230 Received: by CLIFFY.UCS.MUN.CA (LISTSERV-TCP/IP release 14.3) with spool id 28253952 for QUATERNARY@CLIFFY.UCS.MUN.CA; Fri, 9 Oct 2009 15:36:16 -0230 Received: from ella.ucs.mun.ca (mx4.mun.ca [134.153.232.56]) by cliffy.ucs.mun.ca (8.12.11.20060308/8.12.11) with ESMTP id n99HuGxf001263 for <quaternary@cliffy.ucs.mun.ca>; Fri, 9 Oct 2009 15:26:16 -0230 Received: from peterson.ucs.mun.ca (peterson.ucs.mun.ca [134.153.232.35]) by ella.ucs.mun.ca (8.13.1/8.13.1) with ESMTP id n99HuDJ6016693 for <quaternary@cliffy.ucs.mun.ca>; Fri, 9 Oct 2009 15:26:13 -0230 Received: from ellington.ucs.mun.ca (ellington.ucs.mun.ca [134.153.232.51]) by peterson.ucs.mun.ca (8.13.1/8.13.1) with ESMTP id n99Hu9BH026340 for <QUATERNARY@morgan.ucs.mun.ca>; Fri, 9 Oct 2009 15:26:09 -0230 Received: from dnsman.OCE.ORST.EDU (dnsman.OCE.ORST.EDU [128.193.64.33]) by ellington.ucs.mun.ca (8.13.1/8.13.1) with ESMTP id n99Hu5Lu021173 for <QUATERNARY@morgan.ucs.mun.ca>; Fri, 9 Oct 2009 15:26:06 -0230 Received: from pmag.OCE.ORST.EDU (pmag.OCE.ORST.EDU [128.193.65.211]) by dnsman.OCE.ORST.EDU (8.13.6/8.13.6) with ESMTP id n99HuF0x009338 for <QUATERNARY@morgan.ucs.mun.ca>; Fri, 9 Oct 2009 10:56:15 -0700 (PDT) Content-Type: multipart/alternative; boundary=Apple-Mail-7--221690720 Mime-Version: 1.0 (Apple Message framework v936) X-Mailer: Apple Mail (2.936) X-Spam-Flag: NO X-Spam-Checker-Version: SpamAssassin 3.002004 (2008-01-01) X-Spam-Status: No, hits=0.1 required=4.0 tests=HTML_MESSAGE,RECVMORGAN version=3.2.4 X-Spam-Report: 0.1 RECVMORGAN Forged received site * 0.0 HTML_MESSAGE BODY: HTML included in message X-Scanned-By: MIMEDefang 2.67 on 134.153.232.56 X-Scanned-By: MIMEDefang 2.67 on 134.153.232.51 Message-ID: <7D16E0E5-1DA3-4F50-8A20-71D36CC213FC@coas.oregonstate.edu> Date: Fri, 9 Oct 2009 10:54:59 -0700 Reply-To: Sarah Strano <sstrano@COAS.OREGONSTATE.EDU> Sender: Research in Quaternary Science <QUATERNARY@CLIFFY.UCS.MUN.CA> From: Sarah Strano <sstrano@COAS.OREGONSTATE.EDU> Subject: OS Meeting, Session PA05 The role of the North Pacific on climate variability To: QUATERNARY@CLIFFY.UCS.MUN.CA Precedence: list --Apple-Mail-7--221690720 Content-Type: text/plain; charset=WINDOWS-1252; format=flowed Content-Transfer-Encoding: quoted-printable Dear colleagues, We would like to invite submissions to session PA05, =93The role of the North Pacific on climate variability=94 at the upcoming AGU Ocean Sciences Meeting (February 22-26, 2010, in Portland, Oregon, USA). Abstract submissions are due October 15, 2009. Session description: Our understanding of oceanic paleoclimate variability is dominantly based on North Atlantic records. While the North Atlantic clearly plays a critical role in ocean circulation and global climate, we have comparatively little data from the Pacific basin, without which our reconstructions of global paleoclimate processes are incomplete. Findings suggest that the North Pacific is a dynamic region sensitive to externally forced climate change on glacial/interglacial timescales. At the same time, regional processes (e.g. emergence of Beringia, North Pacific Intermediate Water formation, and Aleutian Low dynamics) have the potential to drive global circulation patterns. We invite presentations of new data and model results from the North Pacific and its marginal seas, with insights both into modern climate and ecosystem dynamics, as well as reconstructions of past conditions. Contributions that further clarify the role of the North Pacific on climate from marine, terrestrial, and ice core research groups are encouraged. Invited presenters include Christina Ravelo (UCSC), John Crusius (USGS), Emanuele DiLorenzo (GA Tech), and Joe Ortiz (Kent State). Information on the 2010 Ocean Science meeting: http://www.agu.org/meetings/os10/ Conveners: Sarah Strano, sstrano@coas.oregonstate.edu, Maureen Davies mdavies@coas.oregonstate.edu, Jason Addison ftjaa1@uaf.edu, Summer Praetorius spraetor@coas.oregonstate.edu Please forward this email to anyone else who you think might be interested in this session. Cheers, Sarah Strano Sarah Strano Graduate Student College of Oceanic and Atmospheric Sciences Oregon State University 104 COAS Admin Bldg Corvallis, OR 97331-5503 (541) 737-9351 --Apple-Mail-7--221690720 Content-Type: text/html; charset=WINDOWS-1252 Content-Transfer-Encoding: quoted-printable <html><body style=3D"word-wrap: break-word; -webkit-nbsp-mode: space; = -webkit-line-break: after-white-space; ">Dear colleagues,<br><br>We = would like to invite submissions to session PA05, =93The role of = the<br>&nbsp;North Pacific on climate variability=94 at the = upcoming&nbsp;<span class=3D"il">AGU</span>&nbsp;<span = class=3D"il">Ocean</span><br><span = class=3D"il">Sciences</span>&nbsp;Meeting (February 22-26, 2010, in = Portland, Oregon, USA).<br>Abstract submissions are due October 15, = 2009.<br><br>Session description:<br><br>Our understanding of oceanic = paleoclimate variability is dominantly<br>based on North Atlantic = records. While the North Atlantic clearly &nbsp;plays<br>a critical role = in&nbsp;<span class=3D"il">ocean</span>&nbsp;circulation and global = climate, we have<br>comparatively little data from the Pacific basin, = without which our<br>reconstructions of global paleoclimate processes = are incomplete.<br>Findings suggest that the North Pacific is a dynamic = region sensitive to<br>externally forced climate change on = glacial/interglacial<br>timescales. At the same time, regional processes = (e.g. emergence of<br>Beringia, North Pacific Intermediate Water = formation, and Aleutian Low<br>dynamics) have the potential to drive = global circulation patterns. We<br>invite presentations of new data and = model results from the North<br>Pacific and its marginal seas, with = insights both into modern climate<br>and ecosystem dynamics, as well as = reconstructions of past conditions.<br>Contributions that further = clarify the role of the North Pacific on<br>climate from marine, = terrestrial, and ice core research groups are<br>encouraged. Invited = presenters include Christina Ravelo (UCSC), John<br>Crusius (USGS), = Emanuele DiLorenzo (GA Tech), and Joe Ortiz = (Kent<br>State).<br><br>Information on the 2010&nbsp;<span = class=3D"il">Ocean</span>&nbsp;Science meeting:<br><a = href=3D"http://www.agu.org/meetings/os10/" = target=3D"_blank">http://www.<span = class=3D"il">agu</span>.org/meetings/<wbr>os10/</a><br><br>Conveners: = Sarah Strano,&nbsp;<a = href=3D"mailto:sstrano@coas.oregonstate.edu">sstrano@coas.oregonstate.edu<= /a>, Maureen Davies<br><a = href=3D"mailto:mdavies@coas.oregonstate.edu">mdavies@coas.oregonstate.edu<= /a>,<br>Jason Addison&nbsp;<a = href=3D"mailto:ftjaa1@uaf.edu">ftjaa1@uaf.edu</a>, = Summer<br>Praetorius&nbsp;<a = href=3D"mailto:spraetor@coas.oregonstate.edu">spraetor@coas.oregonstate.ed= u</a><div><br></div><div><a = href=3D"mailto:spraetor@coas.oregonstate.edu"></a></div><div><br>Please = forward this email to anyone else who you think might be<br>interested = in this session.<br><div><div><br></div><div>Cheers,</div><div>Sarah = Strano</div><div><br></div></div></div><div> <span = class=3D"Apple-style-span" style=3D"border-collapse: separate; color: = rgb(0, 0, 0); font-family: Helvetica; font-size: 12px; font-style: = normal; font-variant: normal; font-weight: normal; letter-spacing: = normal; line-height: normal; orphans: 2; text-align: auto; text-indent: = 0px; text-transform: none; white-space: normal; widows: 2; word-spacing: = 0px; -webkit-border-horizontal-spacing: 0px; = -webkit-border-vertical-spacing: 0px; = -webkit-text-decorations-in-effect: none; -webkit-text-size-adjust: = auto; -webkit-text-stroke-width: 0; "><div style=3D"word-wrap: = break-word; -webkit-nbsp-mode: space; -webkit-line-break: = after-white-space; "><span class=3D"Apple-style-span" = style=3D"border-collapse: separate; color: rgb(0, 0, 0); font-family: = Helvetica; font-size: 12px; font-style: normal; font-variant: normal; = font-weight: normal; letter-spacing: normal; line-height: normal; = orphans: 2; text-indent: 0px; text-transform: none; white-space: normal; = widows: 2; word-spacing: 0px; -webkit-border-horizontal-spacing: 0px; = -webkit-border-vertical-spacing: 0px; = -webkit-text-decorations-in-effect: none; -webkit-text-size-adjust: = auto; -webkit-text-stroke-width: 0px; "><div style=3D"word-wrap: = break-word; -webkit-nbsp-mode: space; -webkit-line-break: = after-white-space; "><div><div>Sarah Strano</div><div><div>Graduate = Student</div><div>College of Oceanic and Atmospheric = Sciences</div><div>Oregon State University</div><div>104 COAS Admin = Bldg</div><div>Corvallis, OR 97331-5503</div><div>(541) = 737-9351</div></div></div><div><br></div></div></span><br = class=3D"Apple-interchange-newline"></div></span><br = class=3D"Apple-interchange-newline"> </div><br></body></html>= --Apple-Mail-7--221690720-- ]