Location of long-term mammal monitoring sites and programs. Comes from the Arctic Terrestrial Biodiversity Monitoring Plan is developed to improve the collective ability of Arctic traditional knowledge holders, northern communities and scientists to detect, understand and report on long-term change in Arctic terrestrial ecosystems and biodiversity..

Location of long-term vegetation (including fungi, non-vascular and vascular plants) monitoring sites and programs. Comes from the Arctic Terrestrial Biodiversity Monitoring Plan is developed to improve the collective ability of Arctic traditional knowledge holders, northern communities and scientists to detect, understand and report on long-term change in Arctic terrestrial ecosystems and biodiversity. The report can be seen here http://www.caff.is/publications/view_document/256-arctic-terrestrial-biodiversity-monitoring-plan The monitoring locations are place over the Circumpolar Arctic bioclimate subzones (CAVM Team 2003) http://www.caff.is/flora-cfg/circumpolar-arctic-vegetation-map

Distribution and observed trends of wild Rangifer populations throughout the circumpolar Arctic (from The Circum Arctic Rangifer Monitoring and Assessment Network, CARMA). Note: Wild boreal forest reindeer have not been mapped by CARMA and thus are not represented here. Published in the Arctic Biodiversity Trends 2010 - Selected indicators of change, INDICATOR #02 - released in 2010

A national Canadian Science Advisory Secretariat (CSAS) science advisory process was held in Winnipeg, Manitoba from June 14-17, 2011 to provide science advice on the identification of Ecologically and Biologically Significant Areas (EBSAs) in the Canadian Arctic based on guidance developed by Fisheries and Oceans Canada. This science advisory process focused on the identification of EBSAs within the following marine biogeographic units: the Hudson Bay Complex, the Arctic Basin, the Western Arctic, the Canadian Arctic Archipelago and the Eastern Arctic. Source: <a href="http://www.dfo-mpo.gc.ca/Library/344747.pdf" target="_blank">Fisheries and Oceans Canada</a> Reference: DFO. 2011. Identification of Ecologically and Biologically Significant Areas (EBSA) in the Canadian Arctic. DFO Can. Sci. Advis. Sec. Sci. Advis. Rep. 2011/055. DFO. 2011. Identification of Ecologically and Biologically Significant Areas (EBSAs) in the Canadian Arctic; June 14-17, 2011. DFO Can. Sci. Advis. Sec. Proceed. Ser. 2011/047.

Appendix 3.1 Arctic Terrestrial mammals: Distribution (X = present; Introd = Introduced by humans) by broad geographic region and low or high arctic zones Nomenclature follows D.E. Wilson and D.M. Reeder (eds.) 2005. Mammal Species of the World: a taxonomic and geographic reference. 3rd Ed. Johns Hopkins University Press, Baltimore.

Subdivision of the Arctic into 28 sectors follows mainly the division used in the Pan Arctic Flora (PAF) project. In a few cases some islands are separated from their mainland in the beginning, thus representing very small sectors. Some of them have now been united like in the PAF project, for example Jan Mayen with Arctic Iceland and Bear Island with Svalbard. Others, like the Beringian Islands are still kept separate from the mainland on both sides. - <a href="http://www.caff.is/assessment-series/32-pan-arctic-checklist-of-lichens-and-lichenicolous-fungi" target="_blank"> Pan-Arctic Checklist of Lichens and Lichenicolous Fungi (2011)</a>

Regional divisions of the marine Arctic, as determined by the Marine Expert Monitoring Group of the Circumpolar Biodiversity Monitoring Programme (CBMP). The Circumpolar Marine Biodiversity Monitoring plan identifies eight Arctic Marine Areas where a suite of common parameters, sampling approaches and indicators will be used. Regionally specific parameters may also be applied. Exact boundaries may change over time to reflect changing bio-physical conditions. <a href="http://caff.is/marine/marine-monitoring-publications/3-arctic-marine-biodiversity-monitoring-plan" target="_blank"> Published in the Arctic Marine Biodiversity Monitoring Plan, Chapter 2, page20 - released in 2011 </a>

Boundaries of the geographic area covered by the Arctic Biodiversity Assessment. Includes sub, low and high Arctic bounbaries

The Arctic Terrestrial Biodiversity Monitoring Plan is developed to improve the collective ability of Arctic traditional knowledge holders, northern communities and scientists to detect, understand and report on long-term change in Arctic terrestrial ecosystems and biodiversity.

Satellite-tracked SVP drifting buoys (Sybrandy and Niiler, 1991; Niiler, 2001) provide observations of near-surface circulation at unprecedented resolution. In September 2005, the Global Drifter Array became the first fully realized component of the Global Ocean Observing System when it reached an array size of 1250 drifters. A drifter is composed of a surface float which includes a transmitter to relay data, a thermometer which reads temperature a few centimeters below the air/sea interface, and a submergence sensor used to detect when/if the drogue is lost. The surface float is tethered to a subsurface float which minimizes rectification of surface wave motion (Niiler et al., 1987; Niiler et al., 1995). This in turn is tethered to a holey sock drogue, centered at 15 m depth. The drifter follows the flow integrated over the drogue depth, although some slip with respect to this motion is associated with direct wind forcing (Niiler and Paduan, 1995). This slip is greatly enhanced in drifters which have lost their drogues (Pazan and Niiler, 2000). Drifter velocities are derived from finite differencing their raw position fixes. These velocities, and the concurrent SST measurements, are archived at <a href="http://www.aoml.noaa.gov/phod/dac/dacdata.php" target="_blank">AOML's Drifting Buoy Data Assembly Center</a> where the data are quality controlled and interpolated to 1/4-day intervals (Hansen and Herman, 1989; Hansen and Poulain, 1996). Reference: Lumpkin, R. and Z. Garraffo, 2005: Evaluating the Decomposition of Tropical Atlantic Drifter Observations. J. Atmos. Oceanic Techn. I 22, 1403-1415.