Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Oberbauer, Steven F; Tweedie, Craig E; Welker, Jeff M; Fahnestock, Jace T; Henry, Gregory HR; Webber, Patrick J; Hollister, Robert D; Walker, Marilyn D; Kuchy, Andrea; Elmore, Elizabeth; Starr, Gregory (2007): (Table 1) Climate characteristics of the four North American Tundra Experiment (ITEX) sites [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.817624, Supplement to: Oberbauer, SF et al. (2007): Tundra CO2 fluxes in response to experimental warming across latitudinal and moisture gradients. Ecological Monographs, 77(2), 221-238, https://doi.org/10.1890/06-0649

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
Climate warming is expected to differentially affect CO2 exchange of the diverse ecosystems in the Arctic. Quantifying responses of CO2 exchange to warming in these ecosystems will require coordinated experimentation using standard temperature manipulations and measurements. Here, we used the International Tundra Experiment (ITEX) standard warming treatment to determine CO2 flux responses to growing-season warming for ecosystems spanning natural temperature and moisture ranges across the Arctic biome. We used the four North American Arctic ITEX sites (Toolik Lake, Atqasuk, and Barrow [USA] and Alexandra Fiord [Canada]) that span 10° of latitude. At each site, we investigated the CO2 responses to warming in both dry and wet or moist ecosystems. Net ecosystem CO2 exchange (NEE), ecosystem respiration (ER), and gross ecosystem photosynthesis (GEP) were assessed using chamber techniques conducted over 24-h periods sampled regularly throughout the summers of two years at all sites.
At Toolik Lake, warming increased net CO2 losses in both moist and dry ecosystems. In contrast, at Atqasuk and Barrow, warming increased net CO2 uptake in wet ecosystems but increased losses from dry ecosystems. At Alexandra Fiord, warming improved net carbon uptake in the moist ecosystem in both years, but in the wet and dry ecosystems uptake increased in one year and decreased the other. Warming generally increased ER, with the largest increases in dry ecosystems. In wet ecosystems, high soil moisture limited increases in respiration relative to increases in photosynthesis. Warming generally increased GEP, with the notable exception of the Toolik Lake moist ecosystem, where warming unexpectedly decreased GEP >25%. Overall, the respiration response determined the effect of warming on ecosystem CO2 balance. Our results provide the first multiple-site comparison of arctic tundra CO2 flux responses to standard warming treatments across a large climate gradient. These results indicate that (1) dry tundra may be initially the most responsive ecosystems to climate warming by virtue of strong increases in ER, (2) moist and wet tundra responses are dampened by higher water tables and soil water contents, and (3) both GEP and ER are responsive to climate warming, but the magnitudes and directions are ecosystem-dependent.
Coverage:
Median Latitude: 72.315832 * Median Longitude: -134.885835 * South-bound Latitude: 68.633330 * West-bound Longitude: -157.400000 * North-bound Latitude: 78.880000 * East-bound Longitude: -75.910000
Minimum ELEVATION: m a.s.l. * Maximum ELEVATION: 740 m a.s.l.
Event(s):
ITEX_AF (Alexandra Fiord)  * Latitude: 78.880000 * Longitude: -75.910000 * Elevation: 10.0 m * Location: Ellesmere Island, Canadian Arctic Archipelago * Method/Device: Monitoring station (MONS)
ITEX_AT (Atqasuk)  * Latitude: 70.450000 * Longitude: -157.400000 * Elevation: 30.0 m * Location: Alaska, USA * Method/Device: Monitoring station (MONS)
ITEX_BA (Barrow)  * Latitude: 71.300000 * Longitude: -156.666670 * Elevation: 3.0 m * Location: Barrow, Alaska, USA * Method/Device: Monitoring station (MONS)
Comment:
Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Latitude of eventLatitude
Longitude of eventLongitude
Area/localityAreaOberbauer, Steven F
ELEVATIONElevationm a.s.l.Geocode
Temperature, air, annual meanMAAT°COberbauer, Steven F
Temperature, air, monthly meanTTT monthly m°COberbauer, Steven Ffor July
Precipitation, sumPrecip summmOberbauer, Steven Fsummer (June-August)
CommentCommentOberbauer, Steven F
10 Degree days, thawingTDDOberbauer, Steven F
Size:
20 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Latitude

Longitude

Area

Elevation [m a.s.l.]

MAAT [°C]

TTT monthly m [°C]

Precip sum [mm]

Comment
10 
TDD
ITEX_AF 78.880-75.910Alexandra Fiord, Canada10-14.65.0summer precipitation very infrequent439
ITEX_BA 71.300-156.667Barrow, Alaska, USA3-12.63.757369
ITEX_AT 70.450-157.400Atqasuk, Alaska, USA30-11.99.055618
ITEX_TL 68.633-149.567Toolik Lake, Alaska, USA740-8.611.6180905