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  • 1
    Online Resource
    Online Resource
    ART, Arctic in Transition : science plan ; tThe Arctic in Rapid Transition (ART) is a proposed integrative, multi-disciplinary, long-term pan-Arctic program to study changes and feedbacks with respect to physical characteristics and biogeochemical cycles of the Arctic Ocean and its biological productive capacity (2010)
    Boulder, Colo. : AOSB
    Details Availability
    Keywords: Nordpolarmeer ; Meereskunde ; Klimatologie ; Arktisforschung
    Type of Medium: Online Resource
    Pages: Online-Ressource (PDF-Datei: 34 S., 3,78 MB) , Ill. graph. Darst.
    URL: http://aosb.arcticportal.org/pdf/ART_SciencePlan_04_05_%28full%29.pdf
    Language: English
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    GEOMAR CATALOGUE
    Link to Library Catalog
    get availability status
  • 2
    Electronic Resource
    Electronic Resource
    Recent temperature and precipitation increases in West Siberia and their association with the Arctic Oscillation (2003)
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 22 (2003), S. 0 
    Details
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Surface air temperature and precipitation records for the years 1958-1999 from ten meteorological stations located throughout West Siberia are used to identify climatic trends and determine to what extent these trends are potentially attributable to the Arctic Oscillation (AO). Although recent changes in atmospheric variability are associated with broad Arctic climate change, West Siberia appears particularly susceptible to warming. Furthermore, unlike most of the Arctic, moisture transport in the region is highly variable. The records show that West Siberia is experiencing significant warming and notable increases in precipitation, likely driven, in part, by large-scale Arctic atmospheric variability. Because this region contains a large percentage of the world's peatlands and contributes a significant portion of the total terrestrial freshwater flux to the Arctic Ocean, these recent climatic trends may have globally significant repercussions. The most robust patterns found are strong and prevalent springtime warming, winter precipitation increases, and strong association of non-summer air temperatures with the AO. Warming rates for both spring (0.5-0.8 °C/decade) and annual (0.3-0.5°C/decade) records are statistically significant for nine often stations. On average, the AO is linearly congruent with 96% (winter), 19% (spring), 0% (summer), 67% (autumn) and 53% (annual) of the warming found in this study. Significant trends in precipitation occur most commonly during winter, when four of ten stations exhibit significant increases (4-13 %/decade). The AO may play a lesser role in precipitation variability and is linearly congruent with only 17% (winter), 13% (spring), 12% (summer), 1% (autumn) and 26% (annual) of precipitation trends.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1751-8369.2003.tb00113.x
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    Paper (German National Licenses)
    Fulltext
  • 3
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    Permafrost-Region Lake-DOC version1 Database (PeRL-DOCv1) (2021)
    PANGAEA
    Details
    Publication Date: 2024-05-07
    Description: The pan-Arctic Permafrost-Region Lake-DOC version1 database contains surface water samples of lakes in the permafrost regions of Alaska (49.3 %), Canada (24.2 %), Greenland (3.2 %) and Siberia (23.3 %). It includes concentrations of dissolved organic carbon (DOC) for each of the 1,833 lakes of our synthesis dataset. The lakes of the dataset are located in permafrost regions between 59.2° and 82.5° northern latitude and were sampled between the years 1979 and 2017. We synthesised published datasets and unpublished samples from the author team. We assigned the following information to each lake using existing secondary environmental parameter datasets: - permafrost zone (Brown et al., 1997; Jorgenson et al., 2008), - ecoregion (Olson et al., 2004), - deposit type (Fulton, 1995; Nielsen, 2010; Petrov et al., 2014; Strauss et al., 2016), - ground ice content (Brown et al., 1997; Jorgenson et al., 2008), and - soil organic carbon content (Hugelius et al., 2014). The lakes cover the full range of permafrost extent from the isolated permafrost to continuous permafrost zone. They are located in the boreal forest ecoregion, in the tundra ecoregion and in the boreal-tundra transition zone. For a regionalization we subdivided the data into 13 study areas (22 sites).
    Keywords: 11B; 13B; 13-TY-01_01-2; 13-TY-02_01-2; 13-TY-03_01-2; 13-TY-04_01-2; 13-TY-05_01-2; 13-TY-06; 13-TY-07; 13-TY-08; 13-TY-09; 13-TY-10_01-2; 13-TY-11; 13-TY-12; 13-TY-13; 13-TY-14; 13-TY-15_01-2; 13-TY-16; 13-TY-17; 13-TY-18; 13-TY-19; 13-TY-20; 13-TY-21; 13-TY-22; 13-TY-23; 13-TY-24; 13-TY-25; 13-TY-26_01-2; 13-TY-27_01-2; 13-TY-28_01-2; 13-TY-29_01-2; 13-TY-30_01-2; 13-TY-31_01-2; 13-TY-32_01-2; 14B; 15B; 16B; 16-KP-01-L01_A-B; 16-KP-01-L02-A-B; 16-KP-01-L03-2; 16-KP-01-L04-2; 16-KP-01-L05; 16-KP-02-L06; 16-KP-02-L07; 16-KP-02-L08; 16-KP-02-L09; 16-KP-02-L11; 16-KP-02-L12; 16-KP-02-L13; 16-KP-02-L14; 16-KP-02-L15; 16-KP-02-L16; 16-KP-02-L18; 16-KP-02-L19-2_A-B; 16-KP-02-L20_A-B; 16-KP-02-L22-3; 16-KP-03-L10-1-3; 18B; after NCSCDv2 (Hugelius et al., 2014); AK-Land_2016_NorthwestAlaska; Alaska; Area/locality; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; BAL16-DTLB-CBL; BAL16-DTLB-pond; BAL16-UPL1-W1; BYK16_SW_01; BYK16_SW_02; BYK16_SW_03; BYK16_SW_04; BYK16_SW_06; BYK16_SW_07; BYK16_SW_08; BYK16_SW_09; BYK16_SW_10; BYK16_SW_11; BYK16_SW_12; BYK16_SW_13; BYK16_SW_14; BYK16_SW_15; BYK16_SW_20; BYK16_SW_21; BYK16_SW_22; BYK16_SW_23; BYK16_SW_24; BYK16_SW_25; BYK16_SW_26; BYK16_SW_27; BYK16_SW_28; BYK16_SW_29; BYK16_SW_30; BYK16_SW_31; BYK16_SW_32; BYK16_SW_33; BYK16_SW_34; BYK16_SW_35; BYK16_SW_36; BYK16_SW_37; BYK16_SW_38; BYK16_SW_39; BYK16_SW_40; CA-Land_2012_YukonCoast; CA-Land_2012_YukonCoast_KOM12-H20-2-1m; CA-Land_2012_YukonCoast_LH_2012; CA-Land_2012_YukonCoast_SP_H2O_1-1m; CA-Land_2013_YukonCoast; CA-Land_2013_YukonCoast_11B; CA-Land_2013_YukonCoast_13B; CA-Land_2013_YukonCoast_14B; CA-Land_2013_YukonCoast_15B; CA-Land_2013_YukonCoast_16B; CA-Land_2013_YukonCoast_18B; CA-Land_2014_YukonCoast; CA-Land_2015_YukonCoast; Campaign; Canada; Carbon, organic, dissolved; Changing Permafrost in the Arctic and its Global Effects in the 21st Century; CSP16-L-10-W1; CSP16-L-1-W1; CSP16-L-31-W1; CSP16-L-4-W1; CSP16-L-5-W1; CSP16-L-7-W1; CSP16-SAL-W1; Deposit type; DLP-Pond_14-1; DLP-Pond_14-2; DLP-Pond_14-3; DLP-Pond_14-4; DLP-Pond_14-5; DLP-Pond 14-1; DLP-Pond 14-2; DLP-Pond 14-3; DLP-Pond 14-4; DLP-Pond 14-5; Ecoregion; Event label; Ground ice content, description; HAND; Keperveem_2016; KOB16-T1-W1; KOB16-T2-W1; KOB16-T6-W1; KOB16-T6-W2; KOB16-T6-W3; KOB16-T6-W4; KOB16-T6-W5; KOB16-T7-W1; KOB16-T7-W2; KOB16-T7-W3; KOB16-T7-W4; KOB16-T7-W5; KOB16-UPL1-W1; KOB16-UPL2-W1; KOM12-H20-2-1m; KUR16_W_03; KUR16_W_04; KUR16_W_05; KUR16_W_10; KUR16_W_11; KUR16_W_13; KUR16_W_14; KUR16_W_16; KUR16_W_18; KUR16_W_19; KUR16_W_24; KUR16-W-53; LATITUDE; LD13_A_06; LD13_A_10; LD13_A_12; LD14_A_05; LD14_A_09; LD14_A_11; LD14_A_38; LD14_A_39; LD14_A_72; LD14_A_76; LD14_A_78; LD14_B_01; LD14_B_02; LD14_B_05; LD14_B_06; LD14_B_07; LD14_B_08; LD14_B_09; LD14_B_10; LD14_B_11; LD14_B_12; LD14_B_13; LD14_B_14; LD14_B_15; LD14_B_16; LD14_B_17; LD14_B_18; LD14_B_19; LD14_B_21; LD14_B_22; LD14_B_23; LD14_B_24; LD14_B_25; LD14_B_26; LD14_T_18; LD14_T_21; LD14_T_24; Lena2013; Lena2016_spring, Lena2016_summer; Lena Delta, Siberia, Russia; LH 2012; LK-001; LK-003; LK-004; LK-006; LK-007; LK-008; LK-010; LK-012; LK-013; LK-014; LK-015; LK-016; LK-017; LK-018; LK-019; LK-020; LK-025; LK-026; LK-027; LK-028; LK-029; LK-031; LK-033; LK-034; LONGITUDE; MULT; Multiple investigations; NOA16-T3-W1; NOA16-T3-W2; NOA16-T4-W1; NSP16-DMM-L1-W1; NSP16-DMM-L1-W2; NSP16-NKM-W1; NSP16-PRP-W1; NSP16-RHL-W1; NSP16-SKM-W1; NSP16-TIL-W1; NSP16-UPP-W1; NSP16-W1; NSP16-W2; NSP16-WFM-W1; NSP16-YEP-W1; NUNATARYUK; NUNATARYUK, Permafrost thaw and the changing Arctic coast, science for socioeconomic adaptation; NWAlaska2016; Organic carbon, soil; PAGE21; Permafrost Research; PETA-CARB; Polar Terrestrial Environmental Systems @ AWI; Pond_Micha_Kom_Glas_3; Pond_Micha_Nun_Glas_4; Pond Micha Kom Glas 3; Pond Micha Nun Glas 4; Rapid Permafrost Thaw in a Warming Arctic and Impacts on the Soil Organic Carbon Pool; Reference/source; Region, genetic; RU-Land_2013_Lena; RU-Land_2013_Taymyr; RU-Land_2014_Lena; RU-Land_2015_Yamal; RU-Land_2015_Yamal_LK-001; RU-Land_2015_Yamal_LK-003; RU-Land_2015_Yamal_LK-004; RU-Land_2015_Yamal_LK-006; RU-Land_2015_Yamal_LK-007; RU-Land_2015_Yamal_LK-008; RU-Land_2015_Yamal_LK-010; RU-Land_2015_Yamal_LK-012; RU-Land_2015_Yamal_LK-013; RU-Land_2015_Yamal_LK-014; RU-Land_2015_Yamal_LK-015; RU-Land_2015_Yamal_LK-016; RU-Land_2015_Yamal_LK-017; RU-Land_2015_Yamal_LK-018; RU-Land_2015_Yamal_LK-019; RU-Land_2015_Yamal_LK-020; RU-Land_2015_Yamal_LK-025; RU-Land_2015_Yamal_LK-026; RU-Land_2015_Yamal_LK-027; RU-Land_2015_Yamal_LK-028; RU-Land_2015_Yamal_LK-029; RU-Land_2015_Yamal_LK-031; RU-Land_2015_Yamal_LK-033; RU-Land_2015_Yamal_LK-034; RU-Land_2016_Keperveem; RU-Land_2016_Lena; Sample ID; Sampling by hand; Sampling date; SEL16-T1-W1; SEL16-T2-L1; SEL16-T2-W1; SEL16-T2-W2; Siberia; Site; SOB14_A_16; SOB14_A_31; SOB14_A_32; SOB14_A_33; SOB16_SW_01; SOB16_SW_02; SOB16_SW_03; SOB16_SW_05; SOB16_SW_07; SOB16_SW_08; SOB16_SW_10; SOB16_SW_11; SOB16_SW_12; SOB16_SW_14; SOB16_SW_15; SOB16_SW_16; SP-14-01; SP-14-02; SP-14-03; SP-14-04; SP-14-05; SP-14-06; SP-14-07; SP-14-08; SP-14-09; SP-14-10; SP-14-11; SP-14-12; SP-14-13; SP-14-14; SP-14-15; SP H2O 1-1m; State of permafrost; Taymyr2013; Tschukotka, Sibiria, Russia; Water sampler, UWITEC; WSUWI; Yamal2015; YC15_Pond_KOM; Yukon_Coast_2012; Yukon_Coast_2013; Yukon_Coast_2014; Yukon_Coast_2015
    Type: Dataset
    Format: text/tab-separated-values, 34446 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 4
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    Arctic in Rapid Transition (ART) : integrating priorities for Arctic Marine Science over the next decade (2010)
    In:  [Poster] In: AGU Fall Meeting 2010, 13.12.-17.12..2010, San Francisco, California, USA .
    Details
    Publication Date: 2019-09-23
    Description: GC23E-0960: The Arctic is undergoing rapid environmental and economic transformations. Recent climate warming, which is simplifying access to oil and gas resources, enabling trans-Arctic shipping, and shifting the distribution of harvestable resources, has brought the Arctic Ocean to the top of national and international political agendas. Scientific knowledge of the present status of the Arctic Ocean and the process-based understanding of the mechanics of change are urgently needed to make useful predictions of future conditions throughout the Arctic region. These are required to plan for the consequences of climate change. A step towards improving our capacity to predict future Arctic change was undertaken with the Second International Conference on Arctic Research Planning (ICARP II) meetings in 2005 and 2006, which brought together scientists, policymakers, research managers, Arctic residents, and other stakeholders interested in the future of the Arctic region. The Arctic in Rapid Transition (ART) Initiative developed out of the synthesis of the several resulting ICARP II science plans specific to the marine environment. This process has been driven by the early career scientists of the ICARP II Marine Roundtable. The ART Initiative is an integrative, international, multi-disciplinary, long-term pan-Arctic program to study changes and feedbacks among the physical characteristics and biogeochemical cycles of the Arctic Ocean. The first ART workshop was held in Fairbanks, Alaska in November 2009 with 58 participants. Workshop discussions and reports were used to develop a science plan that integrates, updates, and develops priorities for Arctic Marine Science over the next decade. The science plan was endorsed by endorsed and sponsored by the IASC SSC "Marine System", the former Arctic Ocean Science Board (AOSB). The next step now is to develop the ART Implementation Plan in order to further the goals of ART during the second ART workshop in Winnipeg, Canada. Our focus within the ART Initiative will be to bridge gaps in knowledge not only across disciplinary boundaries (e.g., biology, geochemistry, geology, meteorology, physical oceanography), but also across geographic (e.g., intenational boundaries, shelves, margins, and the central Arctic Ocean) and temporal boundaries (e.g., paleo/geologic records, current process observations, and future modeling studies). This approach of the ART Initiative will provide a means to better understand and predict change, particularly the consequences for biological productivity, and ultimate responses in the Arctic Ocean system. More information about the ART Initiative can be found at http://www.aosb.org/art.html.
    Type: Conference or Workshop Item , NonPeerReviewed
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    OceanRep: Poster
  • 5
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    The Arctic in Rapid Transition (ART) Initiative: integrating priorities for Arctic marine science over the next decade (2011)
    In:  [Poster] In: Arctic Marine Geology and Geophysics Research School Seminar, 15.03.2011, Tromsø, Norway .
    Details
    Publication Date: 2020-10-16
    Type: Conference or Workshop Item , NonPeerReviewed
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    OceanRep: Poster
  • 6
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    Arctic in Rapid Transition (ART): integrating priorities for Arctic marine science of the next decade (2010)
    In:  [Talk] In: UK Polar Network Workshop on Polar Sedimentary Processes and Archives, 18.11.-19.11.2010, Loughborough, UK .
    Details
    Publication Date: 2019-09-23
    Type: Conference or Workshop Item , NonPeerReviewed
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    OceanRep: Talk
  • 7
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    Evaluating the role of Atlantic Water advection to the Arctic Ocean on geological, historical, and observational timescales (2014)
    IUEM
    In:  [Talk] In: ISTAS: Integrating Spatial and Temporal Scales in the Changing Arctic System, 21.10.-24.10.2014, Plouzané, France . ISTAS: Integrating Spatial and Temporal Scales in the Changing Arctic System : Towards Future Research Priorities ; Oct 21 - 24, Plouzané, IUEM ; Book of Abstracts – Plenary Session ; p. 41 .
    Details
    Publication Date: 2019-09-23
    Description: Recent observations of enhanced oceanic heat transfer into the Arctic concomitant with the rapid sea-ice decrease temptingly suggest a direct relationship between both features. However, except for marginal areas of the Arctic Ocean where warm and saline Atlantic Water (AW) reaches the surface, the majority of AW heat is presently isolated from the sea-ice cover by a cold and fresh halocline layer. No evidence has been found to suggest a weakening of the halocline across the central Arctic basins that would enhance the AW heat transfer to the surface. A more direct link between sea-ice reduction and AW inflow is, however, seen in the inflowing Barents Sea branch in both historical and observational time series. In this presentation the AW advection into the Arctic Ocean and its influence on sea-ice variability will be reviewed from a geological point of view. Records from the geologic past are of great value as the time span of modern observations and historical data is often too short to comprehend long-term trends and causes of AW variability, changes in the marginal ice zone, and the vertical structure of the Arctic water column. Paleoceanographic studies from the recent interglacial indirectly suggest that the strength of AW advection and its propagation into the Arctic interior is effective in melting sea ice in combination with other factors such as insolation, sea level, freshwater input, and upper water mass stratification. However, to date, very little paleoceanographic work in the Arctic has focused on how the strength and position of the halocline has changed during previous interglacial periods. More direct reconstructions of the Arctic’s vertical stratification in the geologic past are needed to provide a longer-term view on the stability of the halocline, and more generally, the role of Atlantic Water inflow on the stability of sea ice in the interior basins.
    Type: Conference or Workshop Item , NonPeerReviewed
    Format: text
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    OceanRep: Talk
  • 8
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    Establishing priorities for interdisciplinary Arctic Ocean Science (2010)
    AGU (American Geophysical Union)
    In:  Eos, Transactions American Geophysical Union, 91 . p. 16.
    Details
    Publication Date: 2017-02-10
    Description: Arctic in Rapid Transition (ART) Initiation Workshop; Fairbanks, Alaska, 7–9 November 2009; The Arctic is undergoing rapid environmental and economic transformations. Recent climate warming, which is simplifying access to oil and gas resources, enabling trans-Arctic shipping, and shifting the distribution of harvestable resources, has brought the Arctic Ocean to the top of national and international political agendas. Scientific knowledge of the present status of the Arctic Ocean and a process-based understanding of the mechanisms of change are required to make useful predictions of future conditions throughout the Arctic region. A step toward improving scientists' capacity to predict future Arctic change was undertaken with the Second International Conference on Arctic Research Planning (ICARP II) meeting in 2005 (http://web.arcticportal.org/iasc/icarp). As the ICARP II process came to a close, the Arctic in Rapid Transition (ART) initiative developed out of an effort to synthesize the several ICARP II science plans specific to the Arctic marine environment.
    Type: Article , NonPeerReviewed
    Format: text
    DOI: 10.1029/2010EO160007
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    OceanRep: Article in a Scientific Journal - without review
  • 9
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    The Arctic in Rapid Transition (ART) Initiative: integrating priorities for Arctic marine science over the next decade (2010)
    In:  [Poster] In: State of the Arctic Conference "At the Forefront of Global Change", 16.03.-19.03.2010, Miami, Florida, USA .
    Details
    Publication Date: 2015-02-19
    Description: The Arctic is currently undergoing rapid environmental and economic transformations. Recent and ongoing climate warming which is simplifying access to oil and gas resources, enabling trans-Arctic shipping and shifting the distribution of harvestable resources, has brought the Arctic Ocean to the top of national and international political agendas. Scientific knowledge of the present status of the Arctic Ocean and the process-based understanding needed to make predictions throughout the arctic region are thus urgently required. A step towards improving our capacity to predict future arctic change was undertaken with the Second International Conference on Arctic Research Planning (ICARP II) meetings in 2005 and 2006 which brought together scientists, policymakers, research managers, arctic residents and other stakeholders interested in the future of arctic climate change research. The Arctic in Rapid Transition (ART) Initiative developed out of an effort to synthesize the several resulting ICARP II science plans specific to the marine environment and has been a process driven by the early career scientists of the ICARP II Marine Roundtable. To this end, the ART Initiative is an integrative, international, multi-disciplinary, long-term pan-Arctic program to study changes and feedbacks among the physical characteristics and biogeochemical cycles of the Arctic Ocean and its' resulting capacity for biological productivity. The first ART workshop was held in Fairbanks, Alaska in November 2009 with 58 participants, the results of which will help to develop a science and implementation plan that integrates, updates and develops priorities for arctic marine science over the next decade. Our focus within the ART Initiative will be to bridge gaps in knowledge not only across disciplinary boundaries (e.g., geology, biology, physical oceanography, geochemistry and meteorology), but also across geographic boundaries (e.g., shelves, margins and the central Arctic Ocean) and temporal boundaries (e.g., paleo/geologic records, current process observations and future modeling studies). This interdisciplinary, international and integrated temporal approach of the ART Initiative will provide a means to better understand and predict change and ultimate responses in the Arctic Ocean system. More information about the ART Initiative can be found at www.aosb.org/art.html.
    Type: Conference or Workshop Item , NonPeerReviewed
    Format: text
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    OceanRep: Poster
  • 10
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    Past, present, and future : a science program for the Arctic Ocean linking ancient and contemporary observations of change through modeling. A follow-up to the 2nd International Conference on Arctic Research Planning,19-21 November 2007, Potsdam, Germany (2007)
    AGU (American Geophysical Union)
    In:  Eos, Transactions American Geophysical Union, 88 (28). p. 287.
    Details
    Publication Date: 2017-02-10
    Description: The Arctic Ocean is the missing piece for any global model. Records of processes at both long and short timescales will be necessary to predict the future evolution of the Arctic Ocean through what appears to be a period of rapid climate change. Ocean monitoring is impoverished without the long-timescale records available from paleoceanography and the boundary conditions that can be obtained from marine geology and geophysics. The past and the present are the key to our ability to predict the future.
    Type: Article , NonPeerReviewed
    Format: text
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    OceanRep: Article in a Scientific Journal - without review
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