International Polar Year 2007–2008 - WMO

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Fig. 2.8-6. POLENET autonomous, colocatedcontinuouslyrecording seismic and GPS stations at Wilson Nunatak in Antarctica (a, upper panel). Seismic stations may be installed on snow, whereas GPS require bedrock, a major control on distribution of stations in polar regions. Remote sites are commonly hundreds of kilometers from logistic hubs, requiring longrange aircraft for deployment. Configurations of seismic (b, lower left panel) and GPS (c, lower right panel), show power system components (solar panels, wind turbines and extensive battery banks [in boxes]), Iridium antenna for remote communications with sensors. The GPS site has an ancillary meteorological package installed. (Photos: Antarctic POLENET field team) 280 IPY 20 07–20 08 the polar ice sheets. The new observational data from the POLENET deployments is providing such synoptic data for the first time. Deployments of polar geophysical observatories in the IPY period The label ‘geophysical observatories’ can be applied to large multi-instrument or single-sensor sites, consisting of a variety of instrumentation suites designed to probe the terrestrial and space environments. Here we focus on the IPY POLENET programme, which coordinated observations at permanent stations with remote site deployments of sensors at small stations designed to operate autonomously and record continuously (Fig. 2.8-6). GPS and seismic stations constitute the dominant sensor types in new deployments carried out as part of POLENET during the IPY period. Nevertheless, the POLENET umbrella also includes data acquired at magnetic observatories for earth applications (Cafarella et al., 2008), gravity and absolute gravity stations, tide-gauge sites and other types of geodetic a b c observations. Prior to IPY, continuously-recording GPS and seismic instruments were located at permanent research stations (Antarctica) or inhabited sites (Greenland) (Figs. 2.8-7a and 2.8-7c), relying on the local power grid for operation. Many did not have real-time communications and data were retrieved on a yearly basis. Several SCAR initiatives promoted deployment of remote geophysical observatories in Antarctica. In the time period immediately preceding IPY, many nations deployed GPS and/or seismic stations and arrays at seasonallyoccupied stations and at remote sites away from permanent stations, experimenting with alternative energy sources (Fig. 2.8-6). Many of these stations operated continuously through the summer months and some succeeded with full-year recording. These pioneering efforts led the way for the IPY network deployments. IPY provided the opportunity to bring the Antarctic planning forward and forge international collaborative plans for network deployments. Similar IPY efforts were stimulated in the Arctic region, particularly in Greenland.
Spatially extensive new observatory networks scientifically, targeted new local stations, and upgrades and ongoing maintenance of pre-IPY instrumentation all contributed to the data collection during IPY. The most spectacular advances in network coverage occurred in Greenland and in Antarctica (Fig. 2.8-7) where extensive deployments of autonomous stations at remote sites have been completed. In these regions alone, over 175 remote observatories were installed during the IPY years and 28 nations contributed to the Antarctic and Arctic POLENET effort. More detailed information on the range of activities and national contributions to the program is provided on the POLENET web site (www.polenet. org). In Greenland (Fig. 2.8-7d), a U.S.-led effort carried out in collaboration with Denmark and Luxembourg installed 46 new continuous GPS sites in a network called GNET (Greenland GPS Network) that completely surrounds the bedrock margins of Greenland (Bevis et al., 2009b). Seismic efforts, led by Denmark, continued in Greenland through the IPY and a new internationally-coordinated seismic network, called GLISN (Greenland Ice Sheet Monitoring Network), will deploy new, co-located, autonomous seismic and GPS stations in the coming years (Anderson et al., 2009). In Fennoscandia, the LAPNET (Lapland Network) project deployed ~35 broadband seismometers, complementing existing continuous GPS stations and permanent seismic stations, led by Finland in collaboration with several European nations and Russia (Kozlovskaya and Poutanen, 2006). The HuBLE (Hudson Bay Lithospheric Experiment) overlapped with IPY activities and seismic data from an array of 35 broadband seismometers is providing a data set across part of arctic Canada, with science objectives highly complementary to the POLENET IPY programme (www1.gly.bris. ac.uk/~jmk/HuBLE/home.html). Elsewhere across the Arctic, geodetic and seismic infrastructure maintained by Canada, Denmark, Finland, Norway, Sweden, Russia and the U.S.A. form an important backbone network providing data from regions surrounding the new, embedded network deployments. In West Antarctica (Fig. 2.8-7c), the ANET (Antarctic GPS and seismic Network) project led by the U.S. in collaboration with Canada, Chile, Germany, Italy, Ukraine and the U.K. has installed a network of 29 new continuous GPS and 34 new continuous seismic stations, 18 of which are co-located. Three additional co-located stations and five additional continuous GPS stations will be installed (Fig. 2.8-7c). Additional components of this network on the Antarctic Peninsula include nine new continuous GPS on bedrock from the U.K. CAPGIA (Constraints on Antarctic Peninsula Glacial Isostatic Adjustment) project, six new continuous GPS on bedrock from the U.S.-led LARISSA (Larsen Ice Shelf System, Antarctica) project and new seismic installations by LARISSA and Spain. Other new continuous GPS stations were installed by Germany/ Russia and by Italy to expand the network (Fig. 2.8-7c). In East Antarctica, the GAMSEIS network (Gamburtsev Antarctic Mountains Seismic Experiment), also a component of the AGAP (Antarctica’s Gamburtsev Province) IPY program, led by the U.S. in collaboration with Australia, Canada, China, , Italy, Japan and U.K. (Kanao et al., 2007a,b; Heeszel et al., 2009; Leveque et al., 2010), installed a network of ~40 broadband seismometers on the East Antarctic Ice Sheet (Fig. 2.8-7c). Additional seismic and geodetic installations also took place at inland stations (Leveque et al., 2008; Lombardi et al., 2009). In addition to these new installations, an essential component of the POLENET programme includes continuously-recording geodetic and seismic stations that existed prior to the IPY period (Figs. 2.8-7a and 2.8-7b). These stations contribute data in sectors of the Arctic and Antarctic that are essential to achieve systems-scale polar data coverage. Some stations, for example Japan’s Syowa Station, maintain a critical infrastructure of geodetic measurement systems that supplement GPS. Repeat measurements at absolute gravity stations and related gravity studies are another important POLENET IPY effort in Antarctica (Makinen et al., 2007, 2008; Rogister et al., 2007; Doi et al., 2008). The network of tide gauges in the Antarctica and Arctic provides important data for global sea-level estimates (Craymer et al., 2006; Watson et al., 2008). Research outcomes Seismic and geodetic data must be acquired over a substantial time span for robust analysis to be possible. Data collected during the IPY years is currently undergoing initial analysis; results will be forthcoming over the next few years. Here, selected s C I e n C e P r o g r a m 281
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Understanding Earth’s Polar Chall
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Understanding Earth’s Polar Chall
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iv IPY 20 07-20 08 Table of Content
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vi IPY 20 07-20 08 Preface This sum
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viii IPY 20 07-20 08 Acknowledgemen
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x IPY 20 07-20 08 JC Members, IPO s
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xii IPY 20 07-20 08 Culp, Joseph 3.
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xiv IPY 20 07-20 08 Larsen, Joan Ny
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xvi IPY 20 07-20 08 Virtue, Patti 5
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xviii IPY 20 07-20 08 I N T R O D U
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xx IPY 20 07-20 08 As the polar reg
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xxii IPY 20 07-20 08 from many of t
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xxiv IPY 20 07-20 08
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2 IPY 20 07-20 08 PA R T O N E : PL
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4 IPY 20 07-20 08 References Andree
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Fig. 1.1-1 Carl Weyprecht (1838-188
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8 IPY 20 07-20 08 Box 2 Programme o
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10 IPY 20 07-20 08 Fig. 1.1-4 Globa
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Fig. 1.1-6 First meeting of the Com
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14 IPY 20 07-20 08 at the same Dani
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Fig. 1.1-8 U.S. Navy and constructi
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18 IPY 20 07-20 08 Cooperation.’
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20 IPY 20 07-20 08 decades (1950-19
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22 IPY 20 07-20 08 References Andre
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24 IPY 20 07-20 08 World Data Cente
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26 IPY 20 07-20 08 Placing the Firs
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28 IPY 20 07-20 08 23 Berkner’s l
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Fig. 1.2-1. Report on the forthcomi
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Fig. 1.2-3.First online publication
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34 IPY 20 07-20 08 Box 1 Neumayer D
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Fig. 1.2-7. Fragment from the minut
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38 Box 2 Proposal to Establish an I
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40 IPY 20 07-20 08 the IPY Planning
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42 Box 3 Extract from the Proceedin
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44 Box 4 IPY 20 07-20 08 Resolution
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46 IPY 20 07-20 08 1-12. Paris. IAG
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48 IPY 20 07-20 08 Notes 1 Andreev
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50 IPY 20 07-20 08 nations needed t
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52 IPY 20 07-20 08 ICSU and WMO Pro
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54 IPY 20 07-20 08 Thiede for SCAR,
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56 IPY 20 07-20 08 PG-3, First Disc
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Fig. 1.3-7 (right). Cover page of t
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60 IPY 20 07-20 08 established by 1
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62 IPY 20 07-20 08 Box 3 The develo
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Fig. 1.3-21 (left). Cover page of t
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Fig. 1.3-24. “A Vision for the In
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68 IPY 20 07-20 08 3 To the nine me
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70 IPY 20 07-20 08 multi-disciplina
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Fig. 1.4-2. SCAR Executive Committe
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74 IPY 20 07-20 08 to understand th
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Fig. 1.4-6. Front page of the AOSB
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78 IPY 20 07-20 08 International Po
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80 IPY 20 07-20 08 experts who atte
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82 IPY 20 07-20 08 and recognized I
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84 IPY 20 07-20 08 References IASC
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86 IPY 20 07-20 08 ATCM References
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88 IPY 20 07-20 08 best expertise f
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90 IPY 20 07-20 08 The EoI database
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92 IPY 20 07-20 08 support from Nor
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94 IPY 20 07-20 08 Box 3 Formal est
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96 IPY 20 07-20 08 Fig. 1.5-7. JC C
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98 IPY 20 07-20 08 Fig. 1.5-9. Fahr
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100 IPY 20 07-20 08 Box 7 Global la
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Fig.1.5-16. JC-8 Meeting in St. Pet
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104 IPY 20 07-20 08 Box 8 “The St
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106 IPY 20 07-20 08 A somewhat cont
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Fig.1.5-20 Jerónimo López-Martín
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Fig.1.5-21 IPY 2007-2008 was offici
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112 IPY 20 07-20 08 References Alli
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114 IPY 20 07-20 08 Portugal, Russi
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116 IPY 20 07-20 08 limited success
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118 IPY 20 07-20 08 Fig. 1.6-1. IPO
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120 Box 1 Meetings and conferences
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122 IPY 20 07-20 08 lished under IP
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Fig.1.6-3. IPO staff members Nicola
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126 IPY 20 07-20 08 References Kais
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128 IPY 20 07-20 08 not sufficient
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130 IPY 20 07-20 08 the IPY Observi
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132 IPY 20 07-20 08 and data manage
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134 IPY 20 07-20 08 PA R T T WO: IP
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136 IPY 20 07-20 08 of which have g
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Fig. 2.1-1. The new building of Tik
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140 IPY 20 07-20 08 instruments on
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Fig. 2.1-4. Time-patterns of the da
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Fig. 2.1-6. Ozone loss rates (parts
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146 IPY 20 07-20 08 fractional sea
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148 IPY 20 07-20 08 Fig. 2.1-9. Sea
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150 IPY 20 07-20 08 vations obtaine
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152 IPY 20 07-20 08 pre-dating the
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154 IPY 20 07-20 08 Sensing, 48(4):
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Table 2.2-1. Estimates of volume, h
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Fig. 2.2-3. Track of the NABOS Crui
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Fig. 2.2-4. Distribution of the oce
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162 IPY 20 07-20 08 quality of the
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164 IPY 20 07-20 08 much of the ozo
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166 IPY 20 07-20 08 concentration m
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168 IPY 20 07-20 08 Jackson et al.,
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170 IPY 20 07-20 08 developed or pr
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172 IPY 20 07-20 08 decrease in the
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Fig. 2.2-11. The acoustic data from
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176 IPY 20 07-20 08 providing plent
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178 IPY 20 07-20 08 Sampling of the
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Fig. 2.2-15 The position of the ice
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Fig. 2.2-17. Schematic of the scien
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184 IPY 20 07-20 08 48(1): 5-21. Di
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186 IPY 20 07-20 08 doi:10.1029/200
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Table 2.3-1. IPY projects in the So
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Fig. 2.3-1b. Hydrographic sections
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Fig. 2.3-2a. A total of 61,965 prof
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194 IPY 20 07-20 08 period. These p
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Fig.e 2.3-5. The Weddell gyre flow
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Fig. 2.3-7. Dissolved iron, salinit
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200 IPY 20 07-20 08 Fig. 2.3-8. Ver
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Fig. 2.3-9. CAML ship sampling duri
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204 IPY 20 07-20 08 the theory that
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Fig. 2.3-12. Dead krill on the beac
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Fig. 2.3-14. Laser altimeter swath
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210 IPY 20 07-20 08 tions and Infor
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212 IPY 20 07-20 08 solved iron in
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214 IPY 20 07-20 08 Antarctic ice s
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216 IPY 20 07-20 08 so-called Dansg
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218 IPY 20 07-20 08 other Greenland
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Fig. 2.4-3. The newly completed NEE
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222 IPY 20 07-20 08 In July-August
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Fig. 2.4-7. Bed topography map for
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Fig. 2.4-9. The grid over which dat
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228 IPY 20 07-20 08 Fig. 2.4-10. Ta
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Page 260 and 261: 234 IPY 20 07-20 08 Fig. 2.5-1. Sch
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Page 282 and 283: Fig. 2.7-1. Permafrost extent in th
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Page 286 and 287: Table 2.7-1. Inventory of Northern
Page 288 and 289: Table 2.7-2. Inventory of Antarctic
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Page 300 and 301: Fig. 2.8-1. Antarctica’s Gamburts
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Page 320 and 321: Table 2.9-1. Terrestrial Projects u
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Page 332 and 333: Fig. 2.9-7. Olga Bohuslavova, Ph.D.
Page 334 and 335: 308 IPY 20 07-20 08 Acknowledgement
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Page 338 and 339: Table 2.10-1. List of active projec
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330 IPY 20 07-20 08 popularity duri
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332 IPY 20 07-20 08 in an Arctic Re
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334 IPY 20 07-20 08 Vairo, C., R. C
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Fig. 2.11-1. The circumpolar Arctic
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338 IPY 20 07-20 08 and the Danish
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340 IPY 20 07-20 08 Canadian traini
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342 IPY 20 07-20 08 Fig. 2.11-3. Th
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344 IPY 20 07-20 08 logical studies
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Fig. 2.11-5. Salmon drying on the Y
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348 IPY 20 07-20 08 health status (
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350 IPY 20 07-20 08 communication,
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352 IPY 20 07-20 08 play an importa
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354 IPY 20 07-20 08 References Alle
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356 IPY 20 07-20 08 D are associate
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358 IPY 20 07-20 08 PA R T T H R E
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360 IPY 20 07-20 08 during IPY (Cha
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Fig. 3.1-1. Antarctica mosaic image
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Fig. 3.1-3. Evolution of the Wilkin
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Fig. 3.1-5. Threedimensional mappin
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Fig. 3.1-8. Time series of monthly
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370 IPY 20 07-20 08 References Alli
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Fig. 3.2-1. Potential temperature/
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Fig. 3.2-3. A Distributed Biologica
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Fig. 3.2-4. Fresh water content (FW
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Fig. 3.2-6. Composite changes in th
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Fig. 3.2-7. Mooring components (lef
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382 IPY 20 07-20 08 observing syste
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384 IPY 20 07-20 08 with the recent
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386 IPY 20 07-20 08 ocean circulati
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388 IPY 20 07-20 08 for sustained o
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Fig. 3.3-5. Map showing the locatio
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392 IPY 20 07-20 08 Fig. 3.4-1. Map
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Top left - Fig. 3.4-3: Screen shot
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396 IPY 20 07-20 08 including how t
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Fig. 3.5-1. Antarctic stations at t
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Fig. 3.5-3. Servicing the AWS at Bu
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Fig. 3.5-6. Sonde launch at Halley
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404 IPY 20 07-20 08 Fig. 3.5-8. Bre
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406 IPY 20 07-20 08 Fig. 3.6-1. Ave
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408 IPY 20 07-20 08 forecast ranges
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Fig.3.6-5. Sea Ice Outlook: 2009 Su
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Fig. 3.7-1. Examples of the cryosph
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414 IPY 20 07-20 08 Global Cryosphe
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416 IPY 20 07-20 08 and build on ex
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Fig. 3.8-1. SAON website - www. arc
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420 IPY 20 07-20 08 be necessary to
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422 IPY 20 07-20 08 on data sharing
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424 IPY 20 07-20 08 Fig. 3.9-1. CBM
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Fig. 3.9-3. Screenshots of the CBMP
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Fig. 3.9-5. (left) Data Coverage by
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Table 3.9-2. Current status, trends
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Fig. 3.9-9. The components of a com
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434 IPY 20 07-20 08 CAFF CBMP Repor
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436 IPY 20 07-20 08 polar communiti
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438 IPY 20 07-20 08 Fig. 3.10-3. Mo
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Fig. 3.10-5. Combining data on trad
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Fig. 3.10-6. NOMAD Expedition camp
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444 IPY 20 07-20 08 and visual form
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Fig. 3.10-10. Group of hunters camp
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Fig. 3.10-12. BSSN Research Assista
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Fig. 3.10-15. The Siku- Inuit-Hila
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Fig. 3.10-17. Meeting with officers
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454 IPY 20 07-20 08 monitoring prod
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456 IPY 20 07-20 08 Edited by I. Kr
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458 IPY 20 07-20 08 the World Ocean
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460 IPY 20 07-20 08 In the period l
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Table 3.11-1. National IPY Data Coo
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464 IPY 20 07-20 08 on basic data m
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466 IPY 20 07-20 08 handling commun
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468 IPY 20 07-20 08 funding agencie
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470 IPY 20 07-20 08 metadata. • M
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472 IPY 20 07-20 08 A major initial
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Table 3.11-2. Summary assessment of
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476 IPY 20 07-20 08 tion and Data.F
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478 IPY 20 07-20 08 PA R T F O U R
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480 IPY 20 07-20 08 Fig. 4.0-2. A w
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482 IPY 20 07-20 08 Historical back
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Fig. 4.1-1. Participants at the Str
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486 IPY 20 07-20 08 students throug
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488 IPY 20 07-20 08 Officers from m
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Fig. 4.1-2. Students in Portugal to
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492 IPY 20 07-20 08 Two internation
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494 IPY 20 07-20 08 the submissions
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Fig. 4.1-4. (left) Teachers partici
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498 IPY 20 07-20 08 conference, ‘
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500 Fig. 4.2-1. IPYPD Basic search
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Table 4.2-2. Distribution of public
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504 IPY 20 07-20 08 Google Groups t
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506 IPY 20 07-20 08 tative/liaison
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508 IPY 20 07-20 08 material had to
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510 IPY 20 07-20 08 References Arct
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512 IPY 20 07-20 08 Highlights from
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514 IPY 20 07-20 08 students throug
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Fig. 4.3-1. Participants of the mee
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Fig. 4.3-3. Early career scientists
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520 IPY 20 07-20 08 management. The
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Fig. 4.3-4. During IPY early career
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524 IPY 20 07-20 08 PA R T FI V E :
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526 IPY 20 07-20 08 ‘legacies’)
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528 IPY 20 07-20 08 sciences_for_ip
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530 IPY 20 07-20 08 of multidiscipl
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Fig. 5.1-2 In situ platforms, inclu
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534 IPY 20 07-20 08 tion documented
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536 IPY 20 07-20 08 warming over th
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538 IPY 20 07-20 08 the Russian Ant
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540 IPY 20 07-20 08 Background with
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542 IPY 20 07-20 08 achievements al
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544 IPY 20 07-20 08 with a Sunyaev-
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546 IPY 20 07-20 08 doing will cont
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548 IPY 20 07-20 08 IPY 2007-2008 (
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Fig.5.2-4. Proposed structure of th
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552 IPY 20 07-20 08 from April 2010
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554 IPY 20 07-20 08 References ACIA
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556 IPY 20 07-20 08 and China agree
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Fig.5.3-1. Routine CTD profiling du
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560 IPY 20 07-20 08 Svalbard, Norwa
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Fig.5.3-7. Comparison of geostrophi
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Fig.5.3-9. Participants of the IPY
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Fig.5.3-11. Japanese- Swedish Antar
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Fig.5.3-13. Memorial photo after th
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570 IPY 20 07-20 08 Fig.5.3-15. New
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Fig.5.3-17. Malaysian biologist Che
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Fig.5.3-19. Malaysian Arctic sampli
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576 IPY 20 07-20 08 their role via
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578 IPY 20 07-20 08 IPY 2007-2008 g
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Fig. 5.4-3. Community meeting organ
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582 IPY 20 07-20 08 Krupnik and Jol
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584 IPY 20 07-20 08 training may be
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586 IPY 20 07-20 08 of the universi
Page 614 and 615:
Table 5.4-1: UArctic Members and St
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Fig. 5.4-11. Inaugural IAI meeting
Page 618 and 619:
592 IPY 20 07-20 08 References Refe
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594 IPY 20 07-20 08 Council (AC) in
Page 622 and 623:
596 IPY 20 07-20 08 established in
Page 624 and 625:
598 IPY 20 07-20 08 cal cycle, perm
Page 626 and 627:
600 IPY 20 07-20 08 Fig.5.5-3. In t
Page 628 and 629:
602 IPY 20 07-20 08 New Role of the
Page 630 and 631:
604 IPY 20 07-20 08 Fig. 5.5-6. Ice
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Fig.5.5-8. Paul Berkman, Chair of t
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608 IPY 20 07-20 08 speakers and pa
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610 IPY 20 07-20 08 Approach for Br
Page 638 and 639:
612 IPY 20 07-20 08 promoted since
Page 640 and 641:
614 IPY 20 07-20 08 states in polar
Page 642 and 643:
Fig.5.6-2. The IPY Oslo Science Con
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618 Box 1 Oslo Science Conference P
Page 646 and 647:
Fig. 5.6-6 The inclusion of early c
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622 IPY 20 07-20 08 2008 implementa
Page 650 and 651:
624 IPY 20 07-20 08 capacity buildi
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626 IPY 20 07-20 08 emissions of me
Page 654 and 655:
628 IPY 20 07-20 08 Epilogue Lead A
Page 656 and 657:
Table E-1: What Does It Take to Com
Page 658 and 659:
632 IPY 20 07-20 08 both ICSU and W
Page 660 and 661:
634 IPY 20 07-20 08
Page 662 and 663:
636 IPY 20 07-20 08 Robin Bell is a
Page 664 and 665:
638 IPY 20 07-20 08 Tillmann Mohr i
Page 666 and 667:
640 IPY 20 07-20 08 Volker Rachold
Page 668 and 669:
642 IPY 20 07-20 08 A PPENDIX 2 IPY
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644 IPY 20 07-20 08 Activity ID Tit
Page 672 and 673:
Page 674 and 675:
Page 676 and 677:
650 IPY 20 07-20 08 A PPENDIX 3 Joi
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652 IPY 20 07-20 08 Third Meeting o
Page 680 and 681:
654 IPY 20 07-20 08 Fifth Meeting o
Page 682 and 683:
656 IPY 20 07-20 08 Seventh Meeting
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658 IPY 20 07-20 08 Ninth Meeting o
Page 686 and 687:
660 IPY 20 07-20 08 A PPENDIX 5 Sub
Page 688 and 689:
662 A PPENDIX 6 IPY Project Charts,
Page 690 and 691:
Appendix 6 Fig.3. Version 3.4, Apri
Page 692 and 693:
Appendix 6 Fig.5. Version 6.4, May
Page 694 and 695:
668 A PPENDIX 7 List of the Nationa
Page 696 and 697:
670 IPY 20 07-20 08 Poland IPY Nati
Page 698 and 699:
672 IPY 20 07-20 08 A PPENDIX 9 IPY
Page 700 and 701:
674 IPY 20 07-20 08 2002 February.
Page 702 and 703:
676 IPY 20 07-20 08 January 22. Int
Page 704 and 705:
678 IPY 20 07-20 08 November 24. Ar
Page 706 and 707:
680 IPY 20 07-20 08 March 2. IPY Da
Page 708 and 709:
682 IPY 20 07-20 08 February 16. Sc
Page 710 and 711:
684 IPY 20 07-20 08 2008 January 20
Page 712 and 713:
686 IPY 20 07-20 08 February 26. Th
Page 714 and 715:
688 IPY 20 07-20 08 A PPENDIX 10 Se
Page 716 and 717:
690 IPY 20 07-20 08 A PPENDIX 11 Li
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692 IPY 20 07-20 08 FWC Freshwater
Page 720 and 721:
694 IPY 20 07-20 08 OCH Oscillating
Page 724:
698 The International Polar Year (I
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International Polar Year 2007–2008 - WMO

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