International Polar Year 2007–2008 - WMO

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152 IPY 20 07–20 08 pre-dating the use of leaded gasoline additives, about 90% of Pb deposition was anthropogenic. Clearly, the use of leaded gasoline is only the most recent chapter in a very long history of atmospheric Pb contamination. Since the 1970s, Pb enrichments in snow and firn from Devon Island have gone into decline in response to the gradual elimination of leaded gasoline. Nevertheless, using the natural, background Pb/Sc ratio and Pb isotope data, it is found that at least 90% of the Pb in the High Arctic is still from anthropogenic sources. INterContinental Atmospheric Trans port of Anthropogenic Pollutants to the Arctic (INCATPA, no. 327 www.ec.gc.ca/api-ipy/default. asp?lang=En&n=8EBD7558-1) studied the risks associated with the emissions of POPs and mercury (Hg) in the Pacific region for the contaminant loads in the Arctic. Before IPY, air monitoring of POPs and Hg was performed mainly at Alert, Canada and Ny Ålesund, Norway in the 1990s under AMAP. Hg has also been continuously measured in air at Whistler, B.C. and Amderma, Russia under Environment Canada and Roshydromet for AMAP, respectively. During IPY, air measurements of POPs and/or Hg started at Little Fox Lake, Yukon, Canada; Valkarkai, Russia; Barrow, Dillingham and Fairbanks, Alaska, U.S.A.; Waliguan, Mt. Changbai, Wudalianchi and Xuancheng, China; and Ba Vi, Vietnam. At most stations, these measurements will continue until spring 2010. Soil and air samples were collected along the Chilkoot Trail, Yukon/Alaska, in summer 2007, at different elevations. The purpose is to investigate the atmospheric deposition of POPs and emerging chemicals on mountain ranges in the Kluane National Park, Yukon, Canada. Combined with the air concentration data collected at Little Fox Lake, this work will provide insight on the roles that mountains and forests play in intercepting POPs carried by trans-Pacific air masses. Another project, Atmospheric Monitoring Network for Anthropogenic Pollution in <strong>Polar</strong> Regions (ATMOPOL, no. 76), delivered the first annual data set on POPs in antarctic air. It also studied the influence of climate change on atmospheric distribution patterns of POPs and the identification of new emerging contaminants in arctic environments. INCATPA models simulating the transport and fate of POPs showed that long-range atmospheric transport (LRAT) of POPs from sources in warm latitudes to the Arctic occurs primarily at the midtroposphere. Cold condensation is also likely to occur at the mid-troposphere over a source region in warm low latitudes. The temperature dependent vapour pressures and atmospheric degradation rates of POPs exhibit similarities between the lower atmosphere over the Arctic and the mid-troposphere over a tropical region. Convection over warm latitudes transports the chemicals to a higher altitude where some of them may condense/partition to particles or to the aqueous phase and they become more persistent at the lower temperatures. Strong winds at the mid-troposphere then convey the condensed chemicals also to the Arctic where they can be brought down to the surface by large-scale descending motion and wet deposition. These studies provide a new interpretation on the cold condensation (Arctic trapping) effect and revealed major atmospheric pathways of POPs to the Arctic. POLar study using Aircraft, Remote sensing, surface measurements and model ling of Climate, chemistry, Aerosols and Transport (POLARCAT, no. 32 www.polarcat.no) brought one of the largest atmospheric measurement campaigns ever conducted in the Arctic. Eight research aircraft from the United States, France, Germany, Russia, as well as research groups from many other countries, flew research missions in nearly all parts of the Arctic and sub-Arctic during spring 2007, spring 2008 and summer 2008. The campaigns were coordinated (Fig. 2.1-12) such that comparisons between the different parts of the Arctic can be made. The aircraft missions were complemented by a ship cruise in spring 2008, a railway campaign in Siberia in summer 2008 and measurement campaigns at several Arctic stations (e.g. Summit, Ny Ålesund). They were also supplemented with extensive use of satellite remote sensing products and a large range of different models. Detailed measurements of the gas-phase and particulate-phase chemical composition of the Arctic atmosphere, the optical properties of aerosols, the properties of clouds, etc. were made. In the result, the POLARCAT data set will provide a unique reference for future changes of the Arctic atmosphere. While the data sets are still being processed and analyzed, several research highlights were already published in a POLARCAT special issue in Atmospheric
Chemistry and Physics (www.atmos-chem-phys.net/ special_issue182.html) and elsewhere. A substantial finding was the large influence of both agricultural and forest fires on the aerosol load of the Arctic atmosphere. Already in spring 2008, fires in Kazakhstan and Russia were a major source of Arctic aerosols, even over Alaska. In summer, extensive influence of burning was obvious, too, especially at higher levels in the Arctic atmosphere. References Ångström, A., 1964. The parameters of atmospheric turbidity. Tellus, 16: 64-75. Bodhaine, B.A. and E.G. Dutton, 1993. A long term decrease in Arctic haze at Barrow, Alaska. Geophys. Res. Lett., 20:947-950. Bouchard, A., F. Rabier, V. Guidard and F. Karbou, in press. Enhancements of satellite data assimilation over Antarctica, Monthly Weather Review. Bromwich, D., Y.-H. Kuo, M. Serreze, J. Walsh, L.S. Bai, M. Barlage, K. Hines and A. Slater. 2010. Arctic System Reanalysis: Call for community involvement. EOS Trans. AGU, 91, 13-14. David C., P. Keckhut, A. Armetta, J. Jumelet, M. Marchand and and S. Bekki, 2009. Radiosondes Stratospheric Temperatures from 1957 to 2008 at Dumont d’Urville (Antarctica): trends and link with <strong>Polar</strong> Stratospheric Clouds. Atmos. Chem. Phys. Discuss., 9:25687-25722. Farahani, E. et al., 2009. Features of the Arctic stratosphere during IPY. SPARC Newsletter, 33. Guedj, S., F. Karbou, F. Rabier and A. Bouchard, 2010. Towards a better modeling of surface emissivity to improve AMSU data assimilation over Antarctica. IEEE Trans. in Geosc. and Remote Fig. 2.1-12. The NASA DC8 research aircraft viewed from the DLR Falcon research aircraft during an intercomparison flight over Greenland as part of POLARCAT in summer 2008 (Photo: Hans Schlager, DLR). s C I e n C e P r o g r a m 153
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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
Page 128 and 129: Fig.1.5-16. JC-8 Meeting in St. Pet
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Page 132 and 133: 106 IPY 20 07-20 08 A somewhat cont
Page 134 and 135: Fig.1.5-20 Jerónimo López-Martín
Page 136 and 137: Fig.1.5-21 IPY 2007-2008 was offici
Page 138 and 139: 112 IPY 20 07-20 08 References Alli
Page 140 and 141: 114 IPY 20 07-20 08 Portugal, Russi
Page 142 and 143: 116 IPY 20 07-20 08 limited success
Page 144 and 145: 118 IPY 20 07-20 08 Fig. 1.6-1. IPO
Page 146 and 147: 120 Box 1 Meetings and conferences
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Page 150 and 151: Fig.1.6-3. IPO staff members Nicola
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Page 154 and 155: 128 IPY 20 07-20 08 not sufficient
Page 156 and 157: 130 IPY 20 07-20 08 the IPY Observi
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Page 162 and 163: 136 IPY 20 07-20 08 of which have g
Page 164 and 165: Fig. 2.1-1. The new building of Tik
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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
Page 172 and 173: 146 IPY 20 07-20 08 fractional sea
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
Page 218 and 219: Fig. 2.3-2a. A total of 61,965 prof
Page 220 and 221: 194 IPY 20 07-20 08 period. These p
Page 222 and 223: Fig.e 2.3-5. The Weddell gyre flow
Page 224 and 225: Fig. 2.3-7. Dissolved iron, salinit
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Fig. 2.3-9. CAML ship sampling duri
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204 IPY 20 07-20 08 the theory that
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Fig. 2.3-12. Dead krill on the beac
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Fig. 2.3-14. Laser altimeter swath
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210 IPY 20 07-20 08 tions and Infor
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212 IPY 20 07-20 08 solved iron in
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214 IPY 20 07-20 08 Antarctic ice s
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216 IPY 20 07-20 08 so-called Dansg
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218 IPY 20 07-20 08 other Greenland
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Fig. 2.4-3. The newly completed NEE
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222 IPY 20 07-20 08 In July-August
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Fig. 2.4-7. Bed topography map for
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Fig. 2.4-9. The grid over which dat
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228 IPY 20 07-20 08 Fig. 2.4-10. Ta
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Fig. 2.4-12. Airborne lidar and gro
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232 IPY 20 07-20 08 tic and Antarct
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234 IPY 20 07-20 08 Fig. 2.5-1. Sch
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236 IPY 20 07-20 08 our planet: the
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238 IPY 20 07-20 08 base Syowa via
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240 IPY 20 07-20 08 possible to add
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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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