International Polar Year 2007–2008 - WMO

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Fig. 3.7-1. Examples of the cryosphere. 412 IPY 20 07–20 08 to IPY and to improving our ability to describe the state and fate of the cryosphere. We refer to the IGOS Cryosphere Theme’s goal of a coordinated, robust network of snow and ice measurements as CryOS, the Cryosphere Observing System. Three major workshops were held in Canada, sponsored by the Canadian Space Agency (CSA), Japan co-sponsored by the Japan Aerospace Exploration Agency (JAXA), in cooperation with the Japan Agency for Marine-Earth Science and Technology (JAMSTEC), and the Netherlands sponsored primarily by the European Space Agency (ESA) to engage the scientific and user communities. Input from approximately 100 scientists in 17 countries provided the basis for the IGOS Cryosphere Theme Report. The report is a robust compilation of observing system capabilities, needs and shortcomings, with separate chapters covering the elements of the cryosphere. Specific recommendations for each cryospheric element (e.g., terrestrial snow, ice sheets, permafrost) are listed in the individual chapters of the report. An example for snow is shown in Table 3.7-1. General recommendations are given for the near-, mid- and long-term, with nearterm recommendations focussing on the IPY period. The report was accepted by the IGOS Partners in May 2007, subsequently published with the support of the WMO and first “released” at the Group on Earth Observations (GEO) Plenary Meeting in Capetown, South Africa, November 2007. It has since been widely distributed and has provided the guidance for many IPY initiatives. More information is available at http:// igos-cryosphere.org. The initial phase of CryOS development coincided with IPY. The approach was to engage relevant IPY projects and increase coordination between them with the objective of producing legacy datasets and the capability to extend them continuously after the end of IPY. In this regard, the IGOS Cryosphere Theme team and the collective cryosphere community have been very successful. Accomplishments during IPY include: • an evaluation of current measurement capabilities, observing system requirements and gaps; • a comprehensive set of recommendations in three time frames; • improved coverage of cryospheric elements in the GCOS Implementation Plan and contributions to the GCOS-CEOS (Committee on Earth Observation Satellites) plan for satellite-based products; • efforts to ensure an IPY legacy through the Group on Earth Observations (GEO) Work Plan; • involvement in the satellite mission planning process resulting in the approval of three orbital cycles of coordinated, experimental inter-satellite SAR interferometry, the Global Monitoring for Environment and Security (GMES) Sentinel-1A C-band SAR mission, the GMES Sentinel-3A SAR altimeter mission that will provide sea-ice thickness measurements, RADARSAT Modified Antarctic Mapping Mission (MiniMAMM) SAR mapping of Antarctica and CryoSat-2; • new satellite products for real-time applications, e.g. sea ice concentration, thickness and motion from optical imagers, and a variety of other new satellite products and acquisitions coordinated through Global Interagency IPY Polar Snapshot Year (GIIPSY) project and the IPY Space Task Group (Chapter 3.1); • contributions to the planning of ongoing SCAR scientific research projects including ISMASS (Ice Sheet MASS balance and sea-level), ASPeCT (Antarctic Sea Ice Processes and Climate), PPE (Permafrost and Periglacial Environments) and AGCS (Antarctica in the Global Climate System). The community involvement in CryOS gave it the credibility needed for these accomplishments, the
Parameter C T Measurement Range Measurement Accuracy Resolution Spatial Temporal Comment or Principal O L H U V U V U V U Driver Snow Cover C 20 100 % 15-20 % 1 km day e.g. MODIS T 0 100 % 10 % 0.5 km 1 day Hydromet O 0 100 % 5 % 0.1 km 12 hr Snow Water Equivalent, C 0 0.2 m 2-10 cm 25 km 1 day e.g. AMSR-E satellite (Shallow) T 0 0.3 m 3 cm 0.5 km 6 day Hydromet O 0 0.3 m 2 cm 0.1 km 12 hr Snow Water Equivalent, C none – – – – – – – – Need HF SAR satellite (Deep) T 0.3 3 m 10 % 0.5 km 6 day Hydromet O 0.3 3 m 7 % 0.1 km 12 hr Snow Water Equivalent, in C 0 3 m 1 cm 1 m 30 day Hydromet situ (Shallow) T 0 3 m 1 cm 1 m 7 day Hydromet O 0 3 m 1 cm 1 m 1 day Snow Depth, satellite C 0 -0.7 m 5-35 cm 25 km 1 day e.g. AMSR-E (Shallow) T 0 1 m 10 cm 0.5 km 6 day Hydromet O 0 1 m 6 cm 0.1 km 1 hr Transportation first time this has been done internationally for the cryosphere. The community that started with CliC and SCAR expanded through CryOS. The Cryosphere Theme team has been, and continues to be, an active participant in several related IPY initiatives in which the Theme Report has proved its usefulness as an authoritative source of requirements in cryospheric observations and recommendations on the means to establish them. The Space Task Group for IPY has been an important implementation mechanism for some of the space-based recommendations of the Theme. In particular, the GIIPSY project has worked with space agencies to develop new satellite products and special acquisitions (examples of new satellite products developed for IPY are given on Figs. 3.1-2 and 3.1-6 in Chapter 3.1). The Theme activities and recommendations played an important role in the three IPY Workshops on Sustaining Arctic Observing Networks (SAON) in 2007 and 2008 (Stockholm, Edmonton and Helsinki), as well as in the 2008 U.S.-Canada GEO Workshop on Water and Ice (Washington, D.C.). The Committee on Earth Observation Satellite (CEOS), which was an IGOS Partner and is a GEO Participating Organization, has evaluated a number of potential gap analysis “threads”, where gaps in the observing system were identified by following a thread from a high level question, through products and service, to models and satellite measurements. One of the threads addresses the question “How do changes in the cryosphere impact sea level?” Currently, the Theme is contributing to the Arctic Council’s Snow, Water, Ice and Permafrost in the Arctic (SWIPA) project (www.amap.no), which will produce a report in 2011 on the state of cryosphere in the Arctic. Thus, there is no question that the development of the IGOS Cryosphere Theme has been a worthwhile effort, resulting in a comprehensive assessment of the cryosphere observing system and a significant contributor to other observing system efforts. The development and acceptance of the IGOS-P Cryosphere Theme Report, which provided the conceptual framework for a Cryosphere Observing System (CryOS), may now provide the basis for a more comprehensive, coordinated and integrated cryospheric observing system (Figs. 3.7-2 and 3.7-3) and be a central part of WMO’s new initiative, Global Cryosphere Watch (GCW). Table 3.7-1. A portion of the observational requirements and gaps table for snow, from the IGOS Cryosphere Theme report. o b s e r v I n g s Y s t e m s a n d d a t a m a n a g e m e n t 413
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Understanding Earth’s Polar Chall
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Understanding Earth’s Polar Chall
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iv IPY 20 07-20 08 Table of Content
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vi IPY 20 07-20 08 Preface This sum
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viii IPY 20 07-20 08 Acknowledgemen
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x IPY 20 07-20 08 JC Members, IPO s
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xii IPY 20 07-20 08 Culp, Joseph 3.
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xiv IPY 20 07-20 08 Larsen, Joan Ny
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xvi IPY 20 07-20 08 Virtue, Patti 5
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xviii IPY 20 07-20 08 I N T R O D U
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xx IPY 20 07-20 08 As the polar reg
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xxii IPY 20 07-20 08 from many of t
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xxiv IPY 20 07-20 08
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2 IPY 20 07-20 08 PA R T O N E : PL
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4 IPY 20 07-20 08 References Andree
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Fig. 1.1-1 Carl Weyprecht (1838-188
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8 IPY 20 07-20 08 Box 2 Programme o
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10 IPY 20 07-20 08 Fig. 1.1-4 Globa
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Fig. 1.1-6 First meeting of the Com
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14 IPY 20 07-20 08 at the same Dani
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Fig. 1.1-8 U.S. Navy and constructi
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18 IPY 20 07-20 08 Cooperation.’
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20 IPY 20 07-20 08 decades (1950-19
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22 IPY 20 07-20 08 References Andre
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24 IPY 20 07-20 08 World Data Cente
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26 IPY 20 07-20 08 Placing the Firs
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28 IPY 20 07-20 08 23 Berkner’s l
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Fig. 1.2-1. Report on the forthcomi
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Fig. 1.2-3.First online publication
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34 IPY 20 07-20 08 Box 1 Neumayer D
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Fig. 1.2-7. Fragment from the minut
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38 Box 2 Proposal to Establish an I
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40 IPY 20 07-20 08 the IPY Planning
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42 Box 3 Extract from the Proceedin
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44 Box 4 IPY 20 07-20 08 Resolution
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46 IPY 20 07-20 08 1-12. Paris. IAG
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48 IPY 20 07-20 08 Notes 1 Andreev
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50 IPY 20 07-20 08 nations needed t
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52 IPY 20 07-20 08 ICSU and WMO Pro
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54 IPY 20 07-20 08 Thiede for SCAR,
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56 IPY 20 07-20 08 PG-3, First Disc
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Fig. 1.3-7 (right). Cover page of t
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60 IPY 20 07-20 08 established by 1
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62 IPY 20 07-20 08 Box 3 The develo
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Fig. 1.3-21 (left). Cover page of t
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Fig. 1.3-24. “A Vision for the In
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68 IPY 20 07-20 08 3 To the nine me
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70 IPY 20 07-20 08 multi-disciplina
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Fig. 1.4-2. SCAR Executive Committe
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74 IPY 20 07-20 08 to understand th
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Fig. 1.4-6. Front page of the AOSB
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78 IPY 20 07-20 08 International Po
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80 IPY 20 07-20 08 experts who atte
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82 IPY 20 07-20 08 and recognized I
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84 IPY 20 07-20 08 References IASC
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86 IPY 20 07-20 08 ATCM References
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88 IPY 20 07-20 08 best expertise f
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90 IPY 20 07-20 08 The EoI database
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92 IPY 20 07-20 08 support from Nor
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94 IPY 20 07-20 08 Box 3 Formal est
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96 IPY 20 07-20 08 Fig. 1.5-7. JC C
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98 IPY 20 07-20 08 Fig. 1.5-9. Fahr
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100 IPY 20 07-20 08 Box 7 Global la
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Fig.1.5-16. JC-8 Meeting in St. Pet
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104 IPY 20 07-20 08 Box 8 “The St
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106 IPY 20 07-20 08 A somewhat cont
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Fig.1.5-20 Jerónimo López-Martín
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Fig.1.5-21 IPY 2007-2008 was offici
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112 IPY 20 07-20 08 References Alli
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114 IPY 20 07-20 08 Portugal, Russi
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116 IPY 20 07-20 08 limited success
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118 IPY 20 07-20 08 Fig. 1.6-1. IPO
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120 Box 1 Meetings and conferences
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122 IPY 20 07-20 08 lished under IP
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Fig.1.6-3. IPO staff members Nicola
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126 IPY 20 07-20 08 References Kais
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128 IPY 20 07-20 08 not sufficient
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130 IPY 20 07-20 08 the IPY Observi
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132 IPY 20 07-20 08 and data manage
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134 IPY 20 07-20 08 PA R T T WO: IP
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136 IPY 20 07-20 08 of which have g
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Fig. 2.1-1. The new building of Tik
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140 IPY 20 07-20 08 instruments on
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Fig. 2.1-4. Time-patterns of the da
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Fig. 2.1-6. Ozone loss rates (parts
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146 IPY 20 07-20 08 fractional sea
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148 IPY 20 07-20 08 Fig. 2.1-9. Sea
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150 IPY 20 07-20 08 vations obtaine
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152 IPY 20 07-20 08 pre-dating the
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154 IPY 20 07-20 08 Sensing, 48(4):
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Table 2.2-1. Estimates of volume, h
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Fig. 2.2-3. Track of the NABOS Crui
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Fig. 2.2-4. Distribution of the oce
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162 IPY 20 07-20 08 quality of the
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164 IPY 20 07-20 08 much of the ozo
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166 IPY 20 07-20 08 concentration m
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168 IPY 20 07-20 08 Jackson et al.,
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170 IPY 20 07-20 08 developed or pr
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172 IPY 20 07-20 08 decrease in the
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Fig. 2.2-11. The acoustic data from
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176 IPY 20 07-20 08 providing plent
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178 IPY 20 07-20 08 Sampling of the
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Fig. 2.2-15 The position of the ice
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Fig. 2.2-17. Schematic of the scien
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184 IPY 20 07-20 08 48(1): 5-21. Di
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186 IPY 20 07-20 08 doi:10.1029/200
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Table 2.3-1. IPY projects in the So
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Fig. 2.3-1b. Hydrographic sections
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Fig. 2.3-2a. A total of 61,965 prof
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194 IPY 20 07-20 08 period. These p
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Fig.e 2.3-5. The Weddell gyre flow
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Fig. 2.3-7. Dissolved iron, salinit
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200 IPY 20 07-20 08 Fig. 2.3-8. Ver
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Fig. 2.3-9. CAML ship sampling duri
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204 IPY 20 07-20 08 the theory that
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Fig. 2.3-12. Dead krill on the beac
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Fig. 2.3-14. Laser altimeter swath
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210 IPY 20 07-20 08 tions and Infor
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212 IPY 20 07-20 08 solved iron in
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214 IPY 20 07-20 08 Antarctic ice s
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216 IPY 20 07-20 08 so-called Dansg
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218 IPY 20 07-20 08 other Greenland
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Fig. 2.4-3. The newly completed NEE
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222 IPY 20 07-20 08 In July-August
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Fig. 2.4-7. Bed topography map for
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Fig. 2.4-9. The grid over which dat
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228 IPY 20 07-20 08 Fig. 2.4-10. Ta
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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
Page 388 and 389: Fig. 3.1-1. Antarctica mosaic image
Page 390 and 391: Fig. 3.1-3. Evolution of the Wilkin
Page 392 and 393: Fig. 3.1-5. Threedimensional mappin
Page 394 and 395: Fig. 3.1-8. Time series of monthly
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Page 398 and 399: Fig. 3.2-1. Potential temperature/
Page 400 and 401: Fig. 3.2-3. A Distributed Biologica
Page 402 and 403: Fig. 3.2-4. Fresh water content (FW
Page 404 and 405: Fig. 3.2-6. Composite changes in th
Page 406 and 407: Fig. 3.2-7. Mooring components (lef
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Page 416 and 417: Fig. 3.3-5. Map showing the locatio
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Page 424 and 425: Fig. 3.5-1. Antarctic stations at t
Page 426 and 427: Fig. 3.5-3. Servicing the AWS at Bu
Page 428 and 429: Fig. 3.5-6. Sonde launch at Halley
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Page 436 and 437: Fig.3.6-5. Sea Ice Outlook: 2009 Su
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Page 444 and 445: Fig. 3.8-1. SAON website - www. arc
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Page 450 and 451: 424 IPY 20 07-20 08 Fig. 3.9-1. CBM
Page 452 and 453: Fig. 3.9-3. Screenshots of the CBMP
Page 454 and 455: Fig. 3.9-5. (left) Data Coverage by
Page 456 and 457: Table 3.9-2. Current status, trends
Page 458 and 459: Fig. 3.9-9. The components of a com
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Page 466 and 467: Fig. 3.10-5. Combining data on trad
Page 468 and 469: Fig. 3.10-6. NOMAD Expedition camp
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Page 472 and 473: Fig. 3.10-10. Group of hunters camp
Page 474 and 475: Fig. 3.10-12. BSSN Research Assista
Page 476 and 477: Fig. 3.10-15. The Siku- Inuit-Hila
Page 478 and 479: Fig. 3.10-17. Meeting with officers
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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
Page 656 and 657:
Table E-1: What Does It Take to Com
Page 658 and 659:
632 IPY 20 07-20 08 both ICSU and W
Page 660 and 661:
634 IPY 20 07-20 08
Page 662 and 663:
636 IPY 20 07-20 08 Robin Bell is a
Page 664 and 665:
638 IPY 20 07-20 08 Tillmann Mohr i
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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
Page 672 and 673:
Page 674 and 675:
Page 676 and 677:
650 IPY 20 07-20 08 A PPENDIX 3 Joi
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652 IPY 20 07-20 08 Third Meeting o
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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
Page 724:
698 The International Polar Year (I
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International Polar Year 2007–2008 - WMO

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