International Polar Year 2007–2008 - WMO

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278 IPY 20 07–20 08 Fig. 2.8-5. PLATES & GATES research areas in Antarctica and the Southern Ocean. (Credit: ETOPO2 database, NOAA, National Geophysical Data Center, www.ngdc.noaa.gov/mgg/global/ etopo2.html) timing of shallow- and deep-water opening between the Indian and Pacific Oceans as well as the motion between East and West Antarctica can be better constrained, which is critical to the determination of the timing of the uplift of the Transantarctic Mountains and the evolution of the West Antarctic Rift System. This large-scale continental rift may have played a role as an additional Pacific-Atlantic gateway at times when the submarine-based West Antarctic ice sheet did not exist or retreated entirely. As global and regional bottom-water currents are strongly affected by seafloor morphology, the dynamics of outstanding oceanic plateaus, ridges and fracture zones as well as the varying morphology along continental margins and rises (e.g. development of sedimentary drift deposits) was an additional subject of the PLATES & GATES investigation. The Antarctic Circumpolar Current, for instance, is deviated by the elongated and up to three-kilometer- high basement ridges of the Udintsev and Eltanin Fracture Zone systems in the southern Pacific as well as the Kerguelen Plateau in the southern Indian Ocean. Investigating the crustal and sedimentary transition of the deep water Princess Elizabeth Trough between the shallower southern Kerguelen Plateau and the Antarctic continent was the aim of a specially designed Russian-German two-ship seismic experiment with RV Polarstern and RV Akademic Karpinsky in early 2007. This is just one example of several experiments in the true IPY spirit: a coordinated, multi-national, multi-ship effort with a large science added-value compared to individual experiments. The Russians conducted further extensive geophysical surveys along the continental margin of East Antarctica, which has already resulted in compiled stratigraphic models of the area from the Riiser-Larsen Sea to the eastern Wilkes Land margin (e.g. Leitchenkov et al., 2007). This mapping and interpretation effort
contributes significantly to the New Tectonic Map of Antarctica (Grikurov and Leitchenkov, in press) as part of the IPY PLATES & GATES project. The information on this map, the characterisation of the Antarctic continent-ocean transitions (e.g. Gohl, 2008) and recent regional stratigraphic grids will be compiled in two follow-up, post-IPY projects Circum-Antarctic Stratigraphy and Paleobathymetry (CASP) and Antarctic Paleotopographic Maps (ANTScape). The generation of higher-resolution palaeobathymetric and palaeotopographic grids is a key condition for realistic simulations of palaeo-ocean currents. Within the PLATES & GATES project, Cenozoic and Mesozoic climate reconstructions are performed using a variety of Earth system models designed to evaluate the effect of ocean gateways and basins on palaeo-circulation patterns, the global carbon cycle and nature of polar ice-sheet development. These experiments include sensitivity runs incorporating new palaeobathymetric reconstructions arising from the new data acquisition described above. The results from these experiments are compared with other model simulations, which include different forcing factors such as atmospheric greenhouse gases and mountain uplift to determine the relative importance of palaeogeography on the evolution of polar and global climates over long geological timescales. An international effort PLATES & GATES was set up as a closely knit network project, consisting of 33 individual projects with 46 expeditions, of which 26 expeditions were land-based, 27 were ship-based and 7 were conducted as combined marine-land expeditions. The split between Arctic/sub-Arctic and Antarctic/Southern Ocean expeditions is almost even. The following 16 nations with a total of about 60 scientists, technicians and students were active in funded polar expeditions for this project: Argentina, Chile, Denmark, Germany, Finland, Italy, Japan, New Zealand, Norway, Poland, Russia, Spain, Sweden, U.K., Ukraine and U.S.A.. At least two expeditions were conducted by Chile, Germany, Italy, Norway, Poland, Russia, Spain, Sweden and U.S.A. A summary of all funded PLATES & GATES projects and expeditions can be accessed at www.internationalpolar-year.de/Plates-and-Gates.28.0.html. Although the tectonic evolution of the polar ocean basins and their continental margins has been investigated over the last 40 years in various individual projects, PLATES & GATES is the first coordinated effort to bring together the relevant geoscientific disciplines with the ultimate objective to understand the tectonic and sedimentary processes leading to ocean gateway developments. Also new is the approach to involve the numerical palaeoclimate modelling community, as they are the ones which translate the resulting basin and margin bathymetries and topographies into their dynamic model geometries. The challenge will be to compile this vast amount of data and results from the individual PLATES & GATES projects for more realistic dynamic palaeobathymetric and palaeotopographic grids of geological epochs which were relevant for major events in the Earth’s climate history. At this stage, most collected data and samples are still being analyzed, models are being built and first publications are being written. First initial results were presented at the IPY Open Science Conference 2010 in Oslo. With the abundance of the large variety of data and samples, it will take several years to unify models and describe the processes of polar gateway and basin formation and their effects on long-term climate change. Polar Earth Observing Networks in International Polar Year A dearth of geophysical observations in the polar regions has long been recognized, particularly from sites remote from permanent research stations or inhabited sites. Given the intensive global attention and accelerating research efforts focused on understanding ice sheet behaviour in response to climate change, the establishment of geophysical observing networks during IPY was particularly timely. Fundamental objectives of many of the projects involved in the IPY Polar Earth Observing Network (POLENET) program are focused on measuring solidearth phenomena that provide information on ice mass change and on controls on ice sheet evolution and dynamics. Predictions of the response of the ice sheets to changing global climate, including how ice mass will change, their modes of collapse and the rapidity of resultant sea-level rise, are crucial to planning for our changing environment. Robust predictions require systems-scale observations over s C I e n C e P r o g r a m 279
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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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Page 256 and 257: Fig. 2.4-12. Airborne lidar and gro
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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 306 and 307: Fig. 2.8-6. POLENET autonomous, col
Page 308 and 309: Fig. 2.8-7. Continuouslyrecording G
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Page 320 and 321: Table 2.9-1. Terrestrial Projects u
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Page 324 and 325: Fig. 2.9-2. A small moving drill wa
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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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Page 350 and 351: Fig. 2.10-7. Participants of the
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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
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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
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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
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674 IPY 20 07-20 08 2002 February.
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676 IPY 20 07-20 08 January 22. Int
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678 IPY 20 07-20 08 November 24. Ar
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680 IPY 20 07-20 08 March 2. IPY Da
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682 IPY 20 07-20 08 February 16. Sc
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684 IPY 20 07-20 08 2008 January 20
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686 IPY 20 07-20 08 February 26. Th
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688 IPY 20 07-20 08 A PPENDIX 10 Se
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690 IPY 20 07-20 08 A PPENDIX 11 Li
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692 IPY 20 07-20 08 FWC Freshwater
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694 IPY 20 07-20 08 OCH Oscillating
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698 The International Polar Year (I
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International Polar Year 2007–2008 - WMO

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