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International Polar Year 2007–2008 - WMO

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286<br />

IPY 20 07–20 08<br />

expectations of a ‘step function in activity’ during an<br />

IPY period. For the first time, geophysical observations<br />

of a much greater density and a much larger spatial<br />

scale are available across the polar regions. This<br />

increased observational capacity is the foremost<br />

achievement of the <strong>Polar</strong> Earth Observing Network<br />

during IPY.<br />

Many of the new data are being provided to the<br />

global science community either in near-real-time via<br />

remote communication systems, or shortly after data<br />

is retrieved from remote sites, and is available through<br />

established archiving facilities. As some data sets<br />

remain sequestered, a challenge remains in meeting<br />

IPY data goals. A broader data-sharing agreement<br />

,and compiling project metadata and data access, are<br />

continuing program goals.<br />

Multidisciplinary and interdisciplinary<br />

scientific research<br />

As outlined in previous sections, scientific<br />

investigations on a broad range of topics utilizing the<br />

new polar geophysical observations are underway.<br />

Initial results are beginning to emerge as evidenced<br />

by the large number of studies cited here. Results of<br />

particular societal relevance will include prediction<br />

of mass fluxes of polar ice sheets, improved models<br />

of glacial isostatic adjustment, and better modeling<br />

and prediction of sea-level change. Improved<br />

understanding of continental evolution, plate and<br />

intraplate deformation processes, and feedback<br />

processes between ice sheets and the solid earth, will<br />

provide fundamental new insights into the workings<br />

of the polar and global earth systems. Opportunities<br />

for interdisciplinary studies between communities<br />

studying geophysical, climate, atmospheric and<br />

space weather phenomena are provided by new<br />

data sets from sectors of the polar regions where<br />

few measurements have previously been made. The<br />

synoptic scale and scope of the new observational<br />

data will surely lead to serendipitous scientific<br />

discoveries that we have not yet imagined.<br />

Essential to reaching the full potential for<br />

scientific outcomes of the new observational data<br />

are integrated, multidisciplinary analyses. Examples<br />

include integration of geodetic observations with<br />

complementary seismic imaging studies to place new<br />

and robust constraints on solid-earth ‘rebound’, ice<br />

mass change and the contribution of polar ice sheets<br />

to sea level change, and the integration of geodetic<br />

and seismic investigations of glacial earthquakes<br />

to understand what their signals tell us about ice<br />

dynamics and response of ice sheets to climate<br />

change. Geographical integration, combining results<br />

and insights obtained from both poles, is also vital.<br />

Enhanced modeling capabilities must be developed<br />

to integrate data sets, assimilate the improved<br />

data sets and boundary conditions effectively, and<br />

improve model predictions. Providing a framework for<br />

collaborative, interdisciplinary, international research<br />

is a key future challenge for the POLENET programme.<br />

Technical advances<br />

The major challenges of remote deploy ments in<br />

polar regions are to provide year-round power, including<br />

through the several months of darkness at polar<br />

latitudes, to minimize logistical requirements to reach<br />

and maintain stations at very remote locations, and<br />

to operate the instruments in extreme environmental<br />

conditions. Major advances have been made in these<br />

areas during the IPY period. The U.S. National Science<br />

Foundation invested in technical development for this<br />

type of instrumentation. Detailed information from<br />

this effort on engineering developments for GPS deployments<br />

are found in Willis (2008a,b), Johns (2008),<br />

and online from the UNAVCO facility (http://facility.<br />

unavco.org/project_support/polar/remote/remote.<br />

html). Detailed information on new seismic engineering<br />

developments are provided on line by the<br />

PASSCAL Instrument Center (www.passcal.nmt.edu/<br />

content/polar-programs). Best practices information<br />

for autonomous systems construction, power supplies<br />

and satellite communications are provided via<br />

these websites to the polar science community. Additional<br />

development efforts from many nations and<br />

disciplines are described in abstracts from sessions<br />

on instrumentation development in polar regions<br />

that have been held at international meetings, such<br />

as European Geosciences Union annual assemblies,<br />

throughout the IPY period.<br />

<strong>Polar</strong> outreach and new polar scientists<br />

The POLENET programme has convened a range<br />

of international workshops and thematic sessions<br />

at international geoscience meetings to encourage

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