Title = Thule_Biocomplexity_NMSDsf_NEE_archive
Data Directory = Terrestrial Ecosystems
PI = Dr. Jeff Welker
Enivironment and Natural Resources Institute
707 A Street
University of Alaska Anchorage
Anchorage, AK, 99508
afjmw1@uaa.alaska.edu
907-257-2701
Co PIs = Dr. Josh Schimel
Department of Ecology, Evolution and Marine Biology
Bren Hall, room 4304
University of California, Santa Barbara
Santa Barbara, CA 93106
schimel@lifesci.ucsb.edu
805-893-7688
Dr. Ron Sletten
University of Washington Quaternary Reseach Center
Johnson Hall 363
4000 15th Avenue NE
Seattle,WA 98195-1310
sletten@ess.washington.edu
206-543-0571
Funding Source = NSF Grant # 0221606
Data Set Overview =
Ecosystem carbon dioxide flux measurements were taken at a High Arctic
prostrate dwarf-shrub, herb tunda near Pituffik (Thule), Greenland
(76� 29'N, 68� 26'W; elevation 245 m asl) northwest Greenland.
Between 1978 and 2004, mean annual air temperature and precipitation
for the site were -11.4�C and 12.5 cm respectively. Over the same
period, growing season (June, July and August) air temperatures averaged
3.8�C and approximately 50% of precipitation fell between October and
April as snow. The soil surface of the study site was approximately 40%
covered by vascular plants and 60% unvegetated. Dominant vascular plants
include the deciduous dwarf-shrub Salix arctica, the graminoid Carex
rupestris and the wintergreen dwarf-shrub Dryas integrifolia. The
dataset covers the growing seasons of 2006 and 2007.
The treatments were three levels of winter snow accumulation; ambient
snow (0.25 m), intermediate snow (0.55 m) and deep snow (1.1 m).
The treatments were accomplished by the erection of a 1.2 m snow fence
placed perpendicular to prevailing winds. Snow accumulated behind the
fence in a continuously tapering drift and permanent experimental plots
were located on the ground under the snow depths listed above.
Instrument Descriptions =
Midday carbon dioxide fluxes were measured in each plot (n = 6 per treatment)
using a closed system clear acrylic chamber with an in-line LiCor 6200
infra-red gas analyzer (IRGA; Li-Cor Inc., Lincoln NE) which continuously
monitors CO2 concentration (Vourlitis et al. 1993). Chamber air temperature
and relative humidity were also measured. The clear-chamber flux measurement
technique has previously been used successfully at the study site
(Arens et al. 2008). The IRGA was calibrated using a gas of known CO2
concentration (500 � 2 ppm) on a bi-weekly basis to avoid instrumental error.
Instrumental drift did not exceed a 2 ppm departure from the calibrated value.
Plot-level measurements of 5 and 10 cm soil temperature and volumetric soil
moisture were taken with a VWR Traceable Temperature Probe
(VWR Instruments, West Chester, PA) and a Hydrosense time-domain reflectometry
(TDR) soil moisture probe (Campbell Scientific, Logan, UT), respectively,
during each flux measurement.
Data Collection and Processing =
Carbon dioxide flux data were recorded using the LiCor 6200's internal memory
and were later corrected for changes in chamber microclimate conditions using
the method of Hooper et al. (2002). Net Ecosystem Exchange (NEE) and Ecosystem
Respiration (ER) values were directly measured, while Gross Ecosystem
Photosynthesis (GEP) values were calculated as the difference of NEE and ER
(GEP = NEE - ER). All data were tested for normality and homogenous variance
and were appropriately transformed when these criteria were not met.
Data Format =
The data are tab-delimited ASCII plain text formatted.
References =
Arens SJT, Sullivan PF, Welker JM (2008) Nonlinear responses to nitrogen and strong
interactions with nitrogen and phosphorus additions drastically alter the structure
and function of a high arctic ecosystem. Journal of Geophysical
Research - Biogeosciences, 113, 1-10.
Hooper DU, Cardon ZG, Chapin FS III, Durant M (2002) Corrected calculations for
soil and ecosystem measurements of CO2 using the Li-Cor 6200 Portable Photosynthesis
System. Oecologia, 132, 1-11.
Vourlitis GL, Oechel WC, Hastings SJ, and Jenkins MA (1993) A system for measuring
in situ CO2 and CH4 flux in unmanaged ecosystems: an Arctic example. Functional
Ecology, 7, 36-379.