PPT-Carbon and biogeochemistry of the sea ice zone

Bates et al 2006 Stephens and Keeling 2002 Sigman et al 2010 Takahashi et al 2009 Arrigo et al 2010 McNeil et al 2007 Ventilation and subduction in the sea ice zone Arctic. 500 400 475 575 775 875 1450 1600 450 575 625 825 925 1550 1700 1000 600 675 800 1025 1175 2050 2200 650 775 850 1075 1225 2150 2300 1500 800 875 1025 1275 1475 2650 2800 850 975 1075 1325 1525 2750 2900 2000 1000 1075 1250 1525 1775 3250 3400 1050 1 Bates et al., (2006). Stephens and Keeling (2002). Sigman. et al., (2010). Takahashi et al., (2009). Arrigo. et al., (2010). McNeil et al., (2007). Ventilation and subduction in the sea ice zone. (Arctic). NEON’s 30-year sampling strategy for monitoring ecosystem productivity and biogeochemistry includes co-located measurements of plant structure, biomass, soil and plant biogeochemistry, and microbial populations. The resulting data can be used to address a wide variety of questions related to ecosystem science. This overview focuses on the measurements associated with two specific components of this design: soil biogeochemistry and microbial diversity (page 2), and plant structure and biogeochemistry (page 3). Scaling point measurements of these ecosystem components across space relies heavily on NEON’s Airborne Observation Platform (AOP), which will fly over all NEON sites annually to collect . Features . and the Late . 1990s . Change. Renguang. . Wu. I. nstitute of Atmospheric Physics, . Chinese . Academy of Sciences, Beijing. World . Conference on Climate Change. October . 24-26, . 2016, . Models. :. CanCM3-standard, CanCM3-improved, CanCM4, GEM-NEMO and CFSv2. . Methodology. : . . - hindcast period: 29 years (1982-2010). - 6 months lead-time. . - November and May initiation. The vanishing veneer of frozen ocean isn't just important for polar bears.. By: Russell . McLendon. 11/6/2015. 2. The Arctic hasn't been itself lately. Temperatures there are rising at twice the global rate, sparking an array of changes unlike anything in recorded history. One of the most striking examples is the region's sea ice, whose dramatic decline over the past decade has led to forecasts of an ice-free Arctic Ocean as early as the 2030s. . The Abyssal Zone Created by Shalynn Lee The Abyssal Zone What is it? The Abyssal Z one is 1 out of the 5 pelagic layers in the ocean. This zone contains a very deep depth. “Abyss” comes from the Greek word “ Ice Hockey What is Ice Hockey Ice Hockey is a game played In the Olympics and for a weekend sport. Ice hockey is a very competitive because it is an Olympic sport so more people play ice hockey more often. ndings of the SWIPA project will be disseminated via many scienti"c and public channels during 2010 Julia R. Hagemann. 1,3. , Frank Lamy. 1. , Helge W. Arz. 2. ,. . Lester Lembke-Jene. 1. , Alexandra Auderset. 3,4. , Naomi Harada. 5. , Sze Ling Ho. 6. , Shinya Iwasaki. 7. , Jérôme Kaiser. 2. , Carina B. Lange. 8. th. grade science unit. Source:. http://nsidc.org/cryosphere/seaice/characteristics/formation.html. Arctic or Antarctic. Antarctica- "land surrounded by water“. Arctic - "water surrounded by land" . Navigating. Navigating ocean currents and ice drift. In the past many people did not know that there was ice in the Arctic Ocean or that the ice moved. . We first learned this from finding objects that had drifted across the Arctic.. NASA Goddard Space Flight Center (GSFC). 1. Radar . Waveform Simulations. of Sea Ice Surface Roughness. Li . Li. (202) 767-0849. l. i.li@nrl.navy.mil. Remote Sensing Division. Peter . Gaiser. , David . (Ice Age) Beta Maturity. Cryosphere Products Validation Team. Jeff Key, NOAA/NESDIS/STAR, Team Lead. Paul Meade, Cryosphere Products JAM. DR # 7132. CCR # 474-CCR-13-0945. DRAT discussion: April 19, 2013.