International Polar Year 2007–2008 - WMO

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Fig. 2.3-2a. A total of 61,965 profiles of temperature and salinity were collected by Argo floats during the IPY period (March 2007 – March 2009). (Base map: M. Belbeoch, Argo Information Centre, JCOMMOPS) Fig. 2.3-2 (b). Estimate of density of float distribution. The IPY helped to enhance the coverage of Argo floats in the Southern Ocean, including the deployment of ice-capable floats in the sea ice zone. Nevertheless, the Southern Ocean remains significantly under-sampled (bottom). (Base map: M. Belbeoch, Argo Information Centre, JCOMMOPS) 192 IPY 20 07–20 08
series measurements ever made in these locations. • Process studies were carried out at a number of locations. In particular, the first direct measurements of mixing in the deep Southern Ocean were made during IPY as part of the Diapycnal and Isopycnal Mixing Experiment in the Southern ocean (DIMES) and Southern Ocean FINEstructure (SO-FINE) projects. • Measurements beneath the floating ice shelves and glacier tongues that fringe much of Antarctica were made at several locations. Observations within the sub-ice shelf ocean cavities are very scarce, due to the obvious difficulties of sampling the ocean beneath hundreds of metres of ice. Nevertheless, these measurements are needed to improve understanding of how the interaction between the ocean and the ice shelf can influence the dynamics of the Antarctic ice sheet and how ice shelf melt/ freeze processes modify the ocean water. The AUV Autosub3 made a number of long transits beneath the Pine Island Glacier, where thinning, acceleration and grounding line retreat have been observed by satellites, measuring water properties and the shape of the cavity (Jenkins et al., 2009). Access to the ocean can also be gained by drilling holes through the ice shelf and deploying oceanographic instruments. IPY measurements were made beneath the Amery Ice Shelf (70°E) and Fimbul Ice Shelf (Greenwich Meridian; Lars Smedsrud, pers. com.) as part of ongoing programs. • Long-term sampling programs made a significant contribution to IPY goals, including underway measurements and remote sensing by satellites. Model studies were carried out under the IPY banner and contributed substantially to addressing the scientific questions identified above. Research highlights The unprecedented spatial coverage of IPY observations is providing new insights into the Southern Ocean and its connection to the rest of the globe. The deep hydrographic and tracer sections, Argo floats and animal sensors have delivered a circumpolar snapshot of the state of the Southern Ocean. The IPY repeat hydrographic sections continue time-series established in recent decades, allowing assessment of changes in a variety of parameters throughout the full depth of the Southern Ocean. Such studies have been used to document the uptake of anthropogenic CO 2 by the ocean (e.g. Sabine et al., 2004), and the warming (Johnson and Doney, 2006a,b; Johnson et al., 2007, Fahrbach et al., 2010) and freshening (Aoki et al., 2005; Rintoul, 2007) of Antarctic Bottom Water (AABW). For example, Fig. 2.3-4 shows that freshening of the Adélie Land and Ross Sea sources of AABW, observed in those earlier studies, has continued through the IPY Fig. 2.3-3. Temperature at 200 m depth, as measured by traditional oceanographic platforms and provided by the Coriolis data centre (ships and floats, left) and by seals equipped with oceanographic sensors (right). The seals significantly increase the number of profiles obtained in the sea ice zone in winter (red). (Images: Charassin et al., 2008) s C I e n C e P r o g r a m 193
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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
Page 168 and 169: Fig. 2.1-4. Time-patterns of the da
Page 170 and 171: Fig. 2.1-6. Ozone loss rates (parts
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Page 174 and 175: 148 IPY 20 07-20 08 Fig. 2.1-9. Sea
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Page 182 and 183: Table 2.2-1. Estimates of volume, h
Page 184 and 185: Fig. 2.2-3. Track of the NABOS Crui
Page 186 and 187: Fig. 2.2-4. Distribution of the oce
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Page 194 and 195: 168 IPY 20 07-20 08 Jackson et al.,
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Page 200 and 201: Fig. 2.2-11. The acoustic data from
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Page 204 and 205: 178 IPY 20 07-20 08 Sampling of the
Page 206 and 207: Fig. 2.2-15 The position of the ice
Page 208 and 209: Fig. 2.2-17. Schematic of the scien
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Page 214 and 215: Table 2.3-1. IPY projects in the So
Page 216 and 217: Fig. 2.3-1b. Hydrographic sections
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Page 222 and 223: Fig.e 2.3-5. The Weddell gyre flow
Page 224 and 225: Fig. 2.3-7. Dissolved iron, salinit
Page 226 and 227: 200 IPY 20 07-20 08 Fig. 2.3-8. Ver
Page 228 and 229: Fig. 2.3-9. CAML ship sampling duri
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Page 232 and 233: Fig. 2.3-12. Dead krill on the beac
Page 234 and 235: Fig. 2.3-14. Laser altimeter swath
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Page 246 and 247: Fig. 2.4-3. The newly completed NEE
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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
Page 254 and 255: 228 IPY 20 07-20 08 Fig. 2.4-10. Ta
Page 256 and 257: Fig. 2.4-12. Airborne lidar and gro
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Page 260 and 261: 234 IPY 20 07-20 08 Fig. 2.5-1. Sch
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242 IPY 20 07-20 08 sary environmen
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Fig. 2.6-1. An artist’s cross-sec
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246 IPY 20 07-20 08 conditions. The
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Fig. 2.6-3. Russian scientific trav
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250 IPY 20 07-20 08 Fig. 2.6-5a. Co
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252 IPY 20 07-20 08 Emerging Subgla
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254 IPY 20 07-20 08 Masolov V.N., S
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Fig. 2.7-1. Permafrost extent in th
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258 IPY 20 07-20 08 contributed to
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Table 2.7-1. Inventory of Northern
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Table 2.7-2. Inventory of Antarctic
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264 IPY 20 07-20 08 Arctic Circum-P
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266 IPY 20 07-20 08 Northern Circum
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268 IPY 20 07-20 08 Permafrost in t
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270 IPY 20 07-20 08 Engineers Offic
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272 IPY 20 07-20 08 Valcárcel-Día
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Fig. 2.8-1. Antarctica’s Gamburts
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276 IPY 20 07-20 08 sampling at rel
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278 IPY 20 07-20 08 Fig. 2.8-5. PLA
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Fig. 2.8-6. POLENET autonomous, col
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Fig. 2.8-7. Continuouslyrecording G
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284 IPY 20 07-20 08 Seismic imaging
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286 IPY 20 07-20 08 expectations of
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288 IPY 20 07-20 08 Willis, 2009b.
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290 IPY 20 07-20 08 Meet. Suppl., A
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292 IPY 20 07-20 08 mantle beneath
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Table 2.9-1. Terrestrial Projects u
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296 IPY 20 07-20 08 future. For thi
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Fig. 2.9-2. A small moving drill wa
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300 IPY 20 07-20 08 2.9-4. Field si
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302 IPY 20 07-20 08 line zones have
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304 IPY 20 07-20 08 that the Arctic
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Fig. 2.9-7. Olga Bohuslavova, Ph.D.
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308 IPY 20 07-20 08 Acknowledgement
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310 IPY 20 07-20 08 arctic polar se
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Table 2.10-1. List of active projec
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314 IPY 20 07-20 08 Fig. 2.10-1. IP
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316 IPY 20 07-20 08 Box 1. The ‘f
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318 IPY 20 07-20 08 The field of th
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Table 2.10-2. Recommended ‘Small
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322 IPY 20 07-20 08 as a research a
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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
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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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