PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Consistency of data presented on modern maps of ice cover in the Arctic

Autorzy
Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Information about the condition of ice cover on surface of the water, which are the content of map, are important for carrying out safe navigation and efficient economic activity in the polar regions. Methods of mapping can be fully automated on the basis of developed through years of experience algorithms or additionally supported by experienced professionals. The content of some of those now commonly encountered maps is compiled on the basis of mixed methods. In this work geographic positions of ice maps content are analyzed taking into consideration their usefulness for planning ship’s voyage in ice. The results of this work allow using the contents of studied maps for determining the ship’s route in ice and voyage planning of the ship in ice according to her hull strengthening. The ice maps often have boundary lines for different values of reference. The maximum width of the strips of each boundary line within the Marginal Ice Zone is 100 km. The mean square error of position of the analyzed maps is +/- 2.0 km. Average locations of boundaries are consistent except for GRIB type maps of the OSI SAF and NIS, which seem to indicate much lower value of ice floe concentration. The NIC MIZ maps and S-411 standard maps are consistent for the 13% and 81% concentration. The 40% limits on MASIE maps and 46% limits of concentration on S-411 standard maps are also consistent. The course of ice edge issued by the NIS for the GMDSS METAREA, 19 region visualizes well the boundaries of the area where the ship might encounter any form of ice. Information of the GMDSS METAREA 20 region issued by the AARI represents the average of the limits 1 to 46% of all sources of information, and on average the 13% limit of ice concentration. The one-year old ice limit with thickness of 0.10 to 0.30 meters on the AARI map is consistent with course and average location of boundaries of 81% ice concentration on the NIC MIZ map and S-411 standard map. The multi-year old ice limit of thickness from 0.30 to 2.00 meters on the AARI map is coincident with the 79% limit of concentration displayed on the NIS map.
Rocznik
Strony
55--66
Opis fizyczny
Bibliogr. 18 poz., rys., tab., wykr.
Twórcy
autor
  • Gdynia Maritime University, Faculty of Navigation
Bibliografia
  • Eltoft T., Lavergne T., Dinessen F., Ivanova N., Sandven S., Similä M., Eriksson L., Borenäs K., Lindberg A., Håkansson B.l., Saldo R., Buus-Hinkler J., Dierking W., Doulgeris A., Lavergne T., Mäkynen, Cheng B., Similä M., Hughes N., Berg A., Buus-Hinkler J., Ivanova N., Dierking W., 2011, Nordic Workshop on Radar Remote Sensing of Sea Ice, Chalmers University of Technology, Gothenburg, Sweden 11 & 12 January, 2011, ftp://sidads.colorado.edu/pub/projects/noaa/iicwg/business/Nordic_WS_Proceedings.pdf, accessed 5.03.2016: 58.
  • Erzaty R., Girard-Ardhuin F., Croize-Fillon D., 2007, Sea ice drift in the central arctic using the 89 GHz brightness temperatures of the advanced microwave scanning radiometer, Users manual. Laboratoire d’Océanographie Spatiale, Département d’Océanographie Physique et Spatiale, IFREMER: 20.
  • Gidrometeoizdat, 1974, Nomenclature of sea ice, the symbols for the ice charts [in Russian] (Номенклатура морских карт, условные обозначения для ледовых карт): 77.
  • IHO, 2014, Ice Information Product Specification, JCOMM S-411, Monaco: 47.
  • Jackson C.R., Apel J.R., 2004, Synthetic Aperture Radar Marine User’s Manual. Washington, Department of Commerce, http://www.sarusersmanual. com, accessed 5.03.2016.
  • Mahoney A.R., Barry R.G., Smolyanitsky V., Fetterer F., 2008, Observed sea ice extent in the Russian Arctic, 1933-2006, “Journal of Geophysical Research”, Vol. 113, C11005, doi: 10.1029/2008JC004830.
  • Pastusiak T., 2015, Ship’s route planning in ice infested areas of northern Svalbard following ice charts made by remote sensing methods, Activities in Navigation. Marine navigation and safety of sea transportation, CRC Press, Balkema book, pp. 181-192.
  • Pastusiak T., 2010, Znak lodowy jako element bezpieczeństwa statków w rejonach polarnych,“Prace Wydziału Nawigacyjnego Akademii Morskiej w Gdyni”, Tom 25, pp. 61-70.
  • Rozman P., Hölemann J. A., Krumpen T., Gerdes R., Köberle C., Lavergne T., Adams S., Girard-Ardhuin F., 2011, Validating satellite derived and modelled sea-ice drift in the Laptev Sea with in situ measurements from the winter of 2007/2008, “Polar Research”, Vol. 30 (2011), http://www.polarresearch. net/index.php/polar/article/view/7218, accessed 5.03.2016.
  • Spreen G., Kern S., Stammer D., 2006, Utilization of Multiple Satellite Sensors to Estimate Sea Ice Volume Flux through Fram Strait, in Arctic sea ice thickness: past, present & future, P. Wadhams & G. Amanatidis (eds.), Climate Change and Natural Hazards series 10, European Commission, Brussels, EUR 22416, http://spreen.info/docs/ SpreenEtAl-2006_EU-Book_ArcticSeaIceThickness.pdf, accessed 5.03.2016, pp. 176-192.
  • Sumata H., Lavergne T., Girard-Ardhuin F., Kimura N., Tschudi M. A., Kauker F., Karcher M., Gerdes R., 2014, An intercomparison of Arctic ice drift products to deduce uncertainty estimates, “Journal of Geophys. Res. Oceans”, 119, pp. 4887-4921, doi:10.1002/ 2013JC009724. http://olga.majling.eu/ICE/Sumata-2014-An%20intercomparison%20of%20SIP_r. pdf, accessed 5.03.2016: 35.
  • WMO, 2000, Sea-Ice Information Services in the World. Edition 2000, WMO No. 574.
  • WMO, 2004/1, WMO Colour Code Standards. WMO/ TD-No. 1215, JCOMM Technical Report No. 24:14.
  • WMO, 2004/2, WMO Sea-Ice Nomenclature Terminology. WMO/OMM/ВМО No. 259, Volume 1, Edition 1970 - 2004: 7.
  • WMO, 2005, Sea-Ice Information Services in the World. Edition 2005, WMO No. 574: 100.
  • WMO, 2007, SIGRID-3: A Vector Archive Format for Sea Ice Charts. WMO/TD No. 1214, 2004 (with revisions by ETSI-III, March 2007), JCOMM Technical Report No. 23. Geneva: 75.
  • WMO, 2010/1, Manual on Codes, International Codes. Volume I, (Annex II to WMO Technical Regulations), Part A – Alphanumeric Codes, WMO No. 306: 462.
  • WMO, 2010/2, Sea-Ice Information Services in the World, Edition 2010, WMO No. 574, Geneva:92.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-5677c03a-025d-4f48-a7e1-7747bf4cdd5e
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.