ࡱ> AC@b mjbjb "hhS(((8 .(QSSSSSS,RZ    Q 4"H4|"Q  V@Q UՒ Q0x   Q   Cascadia 2007 and Beyond Slow Slip and Tremor Workshop Motivation and Purpose: The primary purpose of this workshop is to promote collaborative synthesis of all the results of the many different studies of slow slip and tremor in Cascadia from January 2007 to the present. This time period presents an opportunity to elucidate these phenomena with unprecedented resolution, as a result of the new wealth of available observations provided by USArray, PBO installations, the growth of permanent monitoring networks, a number of finite-duration field experiments, and the enthusiasm and vigor of groups that have been analyzing and interpreting these data. The results of these studies are now mature enough to begin exploring how they may fit together. Such exploration has a high likelihood of revealing new behaviors, relationships among and questions about the phenomena of slow slip and tremor, which in turn can stimulate the planning of future field experiments. In addition, this provides the opportunity to demonstrate publicly, through the production of a high-visibility publication, the tremendous pay-off of investing in new instrumentation, infrastructure and collaborative research. Goals: Exchange of research results directly relevant to the understanding of slow slip and tremor in Cascadia from January 2007 to present. Generation of an outline of a high-profile, group-authored manuscript (e.g. a Science Review article) highlighting what has been learned about these phenomena from the wealth of new data and studies, and what new questions they may have motivated. Exchange of information about plans underway and ideas for additional experiments related to the ETS event expected in the summer of 2009. Format, Participants, and Venue: This focused, yet informal, workshop will span two full days during March 2009. We propose the following format: Day 1 Concise presentations of results and current interpretations. Small group discussions (e.g. huddles around laptops or the backs of envelopes to show details of datasets, work out ideas, etc.). Brainstorming about relationships, models, etc. that tie diverse studies together. Day 2 Synthesis of previous day Planning for 2009 ETS event. Manuscript drafting. To be productive, participation needs to be limited in size and scope, to include only those involved in studies that pertain directly to understanding slow slip and tremor in Cascadia since January 2007. Although not a strict limit, a target maximum size is 35 people. Anyone is welcome to apply, with participation allotted on a first-come first-serve basis. Unfortunately, at present all participants must provide their own travel support. PLEASE keep in mind that our goal is to be as inclusive as possible. We plan to make some form of teleconferencing possible for the duration of the workshop, and presence at the workshop is not a requirement for inclusion in authorship of the manuscript we envision (although contribution of ideas, words, editing, etc. will be!). Also, please keep in mind that satisfying all of the workshop goals and constraints may make it impossible to satisfy everyone or to score perfectly on all decisions! The likely venues are the University of Washington campus in Seattle or the DOGAMI facility in Portland (choices made to minimize required travel and expense). Please Respond: If you would like to participate, please send the following information to Evelyn ( HYPERLINK "mailto:evelynr@usgs.gov" evelynr@usgs.gov) or Joan ( HYPERLINK "mailto:gomberg@usgs.gov" gomberg@usgs.gov) by 1/30/09. Preferred location: Seattle or Portland? Dates in March you are NOT available: Sentence or two about your work that relates directly to Cascadia slow slip and tremor from 2007 and beyond: Definitely cannot attend without support (see footnote 2): yes or no?  Both Nature and Science permit self-assigned Group Names to be used for papers in which all authors should be credited equally. If used, all contributing authors also will be listed but the Group Name can be used alone or as the first author. Thus, citations would be to the Group Name or Group Name et al. rather than just using the authors listed alphabetically, for example, in which case the lucky person whose last name just happens to be Aardvark gets lots of citations that no one else does!  If you absolutely cannot attend because of a lack of funds and can provide strong justification that your participation is key, please let us know about both (your need and the justification). There is some possibility that a very small amount of support may be available to help a few participants, with emphasis on possibility and small! 78N !1lm슔jhf0JUhfjhfOJQJUhf0JOJQJjhfOJQJUjhfOJQJUhf6OJQJjhf0JOJQJUhf5OJQJhfOJQJhf5CJOJQJ%78Q ? 8 X ^ tz}~ & Fgdf & F & F & F$a$l~ !12;<bcklm^gdf/ =!"#$%DyK evelynr@usgs.govyK 0mailto:evelynr@usgs.govDyK gomberg@usgs.govyK 0mailto:gomberg@usgs.gov8@8 NormalCJmH sH tH DA@D Default Paragraph FontZi@Z  Table Normal :V 4 l4a _H(k@(No List D@D  Balloon TextCJOJQJaJ:@:  Footnote TextaJ@&@@ Footnote ReferenceH*0U@!0 Hyperlink>*B* mRURUm" z z zm78Q?8X^ tzn0p0p0p0p0p0p 0p 0p 0p0p0p0p0p0p 0p 0p 0p0p 0p y7@78Q?8X^ tz } ~  ! 1 2 ;<bckn0G0G0G0P>0G0G 0G 0P> 0G0G0G0G0P>0G 0G 0G 0P>0G 0G 0P> 0a00a0a0a00a0000000000000a000078Q?8X^ tz } ~  ! 1 2 ;<bckn0p0p0p0pŀ0p0p 0p 0pŀ 0p0p0p0p0pŀ0p 0p 0p 0pŀ0p 0p 0pŀ 0pŀX 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@X 0@000@\00@0m ~ml mXXn n:8-*T$M"jM\6rA؈^`o(. ^`hH. pLp^p`LhH. @ @ ^@ `hH. ^`hH. 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