International Polar Year 2007–2008 - WMO

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Fig. 2.8-1. Antarctica’s Gamburtsev Province (AGAP) IPY project camp locations and aerophysical survey area in East Antarctica. (Image: M. Studinger) 274 IPY 20 07–20 08 the IPY spirit of promoting international cooperation to carry out multi-disciplinary research in a remote area needing very complex logistics (Fig. 2.8-1). AGAP field work during the IPY observational period included the deployment of a network of seismometers at 26 different sites, operating instruments over the Antarctic winter at very low temperatures, and a series of survey flights, covering a total of 120,000 square kilometers, using two aircraft equipped with ice-penetrating radar, gravimeters and magnetic sensors (Fig. 2.8-2). As part of the AGAP survey a seismic experiment was designed to image details of the crust and upper mantle structure across the subglacial range. It consists of the following elements: a) a 900 km linear array of 12 broadband seismic stations; b) an intersecting 550 km linear array of seven broadband seismic stations crossing the Gamburtsev Mountains at an angle of aproximately 115 degrees to the larger line; and c) 8 broadband stations deployed to improve 3-D resolution of the Gamburtsev Mountains survey. More information about the Gamburtsev Antarctic Mountains Seismic Experiment (GAMSEIS) can be obtained on the Web site at Washington University in St. Louis: http://epsc.wustl.edu/seismology/GAMSEIS/ index.html. The new observations have confirmed the existence of a mountain range with a rugged landscape that it is suspected to have been essential in formation of the East Antarctic Ice Sheet. The data confirm earlier findings about the presence of subglacial peaks, valleys, lakes and rivers in a complex water system connected to the ice sheet flow (Bell et al., 2007). AGAP research allows study of the lithosphere structure and uplift history of the Gamburtsev Mountains, located within an intraplate setting, and the role it played in the formation of the East Antarctic Ice Sheet. It has provided inputs into ice sheet, subglacial flow and climate models, and could help to locate the oldest ice core record in the Antarctic Ice Sheet which would be useful for future ice and bedrock drilling. Information about the AGAP project is available at www.ldeo.columbia.edu/agap.
Plate tectonics and polar gateways in the Earth System The thermohaline ocean circulation is an important component in the global climate system. The ocean currents transport heat and matter around the globe and are thus likely to cause global environmental changes. At large geological timescales, the global circulation is affected by geodynamic processes which control the motions of the lithospheric plates as well as crustal uplift and subsidence. Plate tectonic motions have constantly altered the shapes and geometries of the ocean basins and the distribution of land masses. In particular, the geometries of so-called oceanic gateways act as continental bottlenecks in the exchange of water masses between ocean basins and are, therefore, key parameters in simulating palaeo- ocean current systems and palaeoclimate scenarios. The reconstruction of the geometries of ocean gateways, basins and their continental margins feeds into numerical models studying the tectonic effect on climate changes. The IPY lead project PLATES & GATES (no. 77) focuses on tectonic reconstructions and sedimentary processes in Mesozoic and Cenozoic times and, in particular, on the transition from climatic greenhouse to icehouse conditions. For the reconstruction of the oceanographic conditions at times of climate changes, tectonicmagmatic, geodynamic, sedimentary and biostratigraphic processes have been studied in the polar and sub-polar regions. Scientists of 16 nations have been involved in geophysical surveying techniques, tectonic measurements and sedimentary Fig. 2.8-2. Methods in the exploration of the subglacial Gamburtsev Mountains. (Image: British Antarctic Survey) s C I e n C e P r o g r a m 275
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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
Page 250 and 251: Fig. 2.4-7. Bed topography map for
Page 252 and 253: Fig. 2.4-9. The grid over which dat
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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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Fig. 2.10-7. Participants of the
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Fig. 2.10-9. 6th International Cong
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328 IPY 20 07-20 08 eral models. Th
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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
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Table 5.4-1: UArctic Members and St
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Fig. 5.4-11. Inaugural IAI meeting
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592 IPY 20 07-20 08 References Refe
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594 IPY 20 07-20 08 Council (AC) in
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596 IPY 20 07-20 08 established in
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598 IPY 20 07-20 08 cal cycle, perm
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600 IPY 20 07-20 08 Fig.5.5-3. In t
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602 IPY 20 07-20 08 New Role of the
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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
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612 IPY 20 07-20 08 promoted since
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614 IPY 20 07-20 08 states in polar
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Fig.5.6-2. The IPY Oslo Science Con
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618 Box 1 Oslo Science Conference P
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Fig. 5.6-6 The inclusion of early c
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622 IPY 20 07-20 08 2008 implementa
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624 IPY 20 07-20 08 capacity buildi
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626 IPY 20 07-20 08 emissions of me
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628 IPY 20 07-20 08 Epilogue Lead A
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Table E-1: What Does It Take to Com
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632 IPY 20 07-20 08 both ICSU and W
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634 IPY 20 07-20 08
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636 IPY 20 07-20 08 Robin Bell is a
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638 IPY 20 07-20 08 Tillmann Mohr i
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640 IPY 20 07-20 08 Volker Rachold
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642 IPY 20 07-20 08 A PPENDIX 2 IPY
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644 IPY 20 07-20 08 Activity ID Tit
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650 IPY 20 07-20 08 A PPENDIX 3 Joi
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652 IPY 20 07-20 08 Third Meeting o
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654 IPY 20 07-20 08 Fifth Meeting o
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656 IPY 20 07-20 08 Seventh Meeting
Page 684 and 685:
658 IPY 20 07-20 08 Ninth Meeting o
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660 IPY 20 07-20 08 A PPENDIX 5 Sub
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662 A PPENDIX 6 IPY Project Charts,
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Appendix 6 Fig.3. Version 3.4, Apri
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Appendix 6 Fig.5. Version 6.4, May
Page 694 and 695:
668 A PPENDIX 7 List of the Nationa
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670 IPY 20 07-20 08 Poland IPY Nati
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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
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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
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688 IPY 20 07-20 08 A PPENDIX 10 Se
Page 716 and 717:
690 IPY 20 07-20 08 A PPENDIX 11 Li
Page 718 and 719:
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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