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CA-SF2: Saskatchewan - Western Boreal, forest burned in 1989

Tower_team:
PI: Brian Amiro Brian_Amiro@umanitoba.ca - University of Manitoba
Lat, Long: 54.2539, -105.8775
Elevation(m): 520
Network Affiliations: AmeriFlux, Fluxnet-Canada
Vegetation IGBP: ENF (Evergreen Needleleaf Forests: Lands dominated by woody vegetation with a percent cover >60% and height exceeding 2 meters. Almost all trees remain green all year. Canopy is never without green foliage.)
Climate Koeppen: Dfc (Subarctic: severe winter, no dry season, cool summer)
Mean Annual Temp (°C): 0.4
Mean Annual Precip. (mm): 470
Flux Species Measured: CO2
Years Data Collected: 2001 - 2005
Years Data Available:

AmeriFlux BASE 2001 - 2006   Data Citation

AmeriFlux FLUXNET 2001 - 2006   Data Citation
Data Use Policy:AmeriFlux CC-BY-4.0 Policy1
Description:
Amiro_et_al_2006, AFM/136:...The 1989 burn site (F89) was northeast of Prince Albert National Park, Saskatchewan, with the humancaused fire covering 13,500 ...
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URL: —
Research Topics: —
Acknowledgment: The data collection was funded by the Canadian Forest Service (Natural Resources Canada) and by Parks Canada as part of the BERMS (Boreal Ecosystem Research and Monitoring Sites) initiative in collaboration with the Fluxnet Canada Research Network and the Canadian Carbon Program (supported by the Canadian National Science and Engineering Research Council (NSERC), the Canadian Foundation for Climate and Atmospheric Sciences and the BIOCAP Canada Foundation).
Site Tasks
  1. This site’s data can also be used under the more restrictive AmeriFlux Legacy Policy.
    The AmeriFlux Legacy Policy must be followed if this site’s data are combined with data from sites that require the AmeriFlux Legacy Policy.
Site Photo More Site Images
Image Credit: , 09/13/2002
Copyright preference: Open use
Site Publication More Site Publications

CA-SF2: Saskatchewan - Western Boreal, forest burned in 1989

Use the information below for citation of this site. See the Data Policy page for more details.

DOI(s) for citing CA-SF2 data

Data Use Policy: AmeriFlux CC-BY-4.0 License

This site’s data can also be used under the more restrictive AmeriFlux Legacy Policy.
The AmeriFlux Legacy Policy must be followed if CA-SF2 data are combined with data from sites that require the AmeriFlux Legacy Policy.

  • AmeriFlux BASE: https://doi.org/10.17190/AMF/1246007
    Citation: Brian Amiro (2019), AmeriFlux BASE CA-SF2 Saskatchewan - Western Boreal, forest burned in 1989, Ver. 3-5, AmeriFlux AMP, (Dataset). https://doi.org/10.17190/AMF/1246007
  • AmeriFlux FLUXNET: https://doi.org/10.17190/AMF/2006961
    Citation: Brian Amiro (2023), AmeriFlux FLUXNET-1F CA-SF2 Saskatchewan - Western Boreal, forest burned in 1989, Ver. 3-5, AmeriFlux AMP, (Dataset). https://doi.org/10.17190/AMF/2006961

Find global FLUXNET datasets, like FLUXNET2015 and FLUXNET-CH4, and their citation information at fluxnet.org.

To cite BADM when downloaded on their own, use the publications below for citing site characterization. When using BADM that are downloaded with AmeriFlux BASE and AmeriFlux FLUXNET products, use the DOI citation for the associated data product.

Publication(s) for citing site characterization

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Acknowledgments

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Resources

CA-SF2: Saskatchewan - Western Boreal, forest burned in 1989

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CA-SF2: Saskatchewan - Western Boreal, forest burned in 1989

Year Publication
2020 Xu, B., Arain, M. A., Black, T. A., Law, B. E., Pastorello, G. Z., Chu, H. (2020) Seasonal Variability Of Forest Sensitivity To Heat And Drought Stresses: A Synthesis Based On Carbon Fluxes From North American Forest Ecosystems, Global Change Biology, 26(2), 901-918. https://doi.org/10.1111/gcb.14843
2021 Chu, H., Luo, X., Ouyang, Z., Chan, W. S., Dengel, S., Biraud, S. C., Torn, M. S., Metzger, S., Kumar, J., Arain, M. A., Arkebauer, T. J., Baldocchi, D., Bernacchi, C., Billesbach, D., Black, T. A., Blanken, P. D., Bohrer, G., Bracho, R., Brown, S., Brunsell, N. A., Chen, J., Chen, X., Clark, K., Desai, A. R., Duman, T., Durden, D., Fares, S., Forbrich, I., Gamon, J. A., Gough, C. M., Griffis, T., Helbig, M., Hollinger, D., Humphreys, E., Ikawa, H., Iwata, H., Ju, Y., Knowles, J. F., Knox, S. H., Kobayashi, H., Kolb, T., Law, B., Lee, X., Litvak, M., Liu, H., Munger, J. W., Noormets, A., Novick, K., Oberbauer, S. F., Oechel, W., Oikawa, P., Papuga, S. A., Pendall, E., Prajapati, P., Prueger, J., Quinton, W. L., Richardson, A. D., Russell, E. S., Scott, R. L., Starr, G., Staebler, R., Stoy, P. C., Stuart-Haëntjens, E., Sonnentag, O., Sullivan, R. C., Suyker, A., Ueyama, M., Vargas, R., Wood, J. D., Zona, D. (2021) Representativeness Of Eddy-Covariance Flux Footprints For Areas Surrounding Ameriflux Sites, Agricultural And Forest Meteorology, 301-302, 108350. https://doi.org/10.1016/j.agrformet.2021.108350
2018 Baldocchi, D., Penuelas, J. (2018) The Physics And Ecology Of Mining Carbon Dioxide From The Atmosphere By Ecosystems, Global Change Biology, . https://doi.org/10.1111/gcb.14559
2009 Amiro, B. (2009) Measuring Boreal Forest Evapotranspiration Using The Energy Balance Residual, Journal Of Hydrology, 366(1-4), 112-118. https://doi.org/10.1016/j.jhydrol.2008.12.021
2006 Amiro, B., Orchansky, A., Barr, A., Black, T., Chambers, S., Chapin III, F., Goulden, M., Litvak, M., Liu, H., McCaughey, J., McMillan, A., Randerson, J. (2006) The Effect Of Post-Fire Stand Age On The Boreal Forest Energy Balance, Agricultural And Forest Meteorology, 140(1-4), 41-50. https://doi.org/10.1016/j.agrformet.2006.02.014
2010 Amiro, B.D., Barr, A.G., Barr, J.G., Black, T.A., Bracho, R., Brown, M., Chen, J., Clark, K.L., Davis, K.J., Desai, A.R., Dore, S., Engel, V., Fuentes, J.D., Goldstein, A.H., Goulden, M.L., Kolb, T.E., Lavigne, M.B., Law, B.E., Margolis, H.A., Martin, T., McCaughey, J.H., Misson, L., Montes-Helu, M., Noormets, A., Randerson, J.T., Starr, G., Xiao, J. (2010) Ecosystem Carbon Dioxide Fluxes After Disturbance In Forests Of North America, Journal Of Geophysical Research, 115(G00K02), n/a-n/a. https://doi.org/10.1029/2010jg001390
2001 Amiro, B. D. (2001) Paired-Tower Measurements Of Carbon And Energy Fluxes Following Disturbance In The Boreal Forest, Global Change Biology, 7(3), 253-268. https://doi.org/10.1046/j.1365-2486.2001.00398.x
1999 Rayment, M. B., Jarvis, P. G. (1999) Seasonal Gas Exchange Of Black Spruce Using An Automatic Branch Bag System, Canadian Journal Of Forest Research, 29(10), 1528-1538. https://doi.org/10.1139/cjfr-29-10-1528
2003 Amiro, B. D., Ian MacPherson, J., Desjardins, R. L., Chen, J. M., Liu, J. (2003) Post-Fire Carbon Dioxide Fluxes In The Western Canadian Boreal Forest: Evidence From Towers, Aircraft And Remote Sensing, Agricultural And Forest Meteorology, 115(1-2), 91-107. https://doi.org/10.1016/s0168-1923(02)00170-3
2009 Mkhabela, M., Amiro, B., Barr, A., Black, T., Hawthorne, I., Kidston, J., McCaughey, J., Orchansky, A., Nesic, Z., Sass, A., Shashkov, A., Zha, T. (2009) Comparison Of Carbon Dynamics And Water Use Efficiency Following Fire And Harvesting In Canadian Boreal Forests, Agricultural And Forest Meteorology, 149(5), 783-794. https://doi.org/10.1016/j.agrformet.2008.10.025
2006 Amiro, B., Barr, A., Black, T., Iwashita, H., Kljun, N., Mccaughey, J., Morgenstern, K., Murayama, S., Nesic, Z., Orchansky, A. (2006) Carbon, Energy And Water Fluxes At Mature And Disturbed Forest Sites, Saskatchewan, Canada, Agricultural And Forest Meteorology, 136(3-4), 237-251. https://doi.org/10.1016/j.agrformet.2004.11.012
2010 Amiro, B. (2010) Estimating Annual Carbon Dioxide Eddy Fluxes Using Open-Path Analysers For Cold Forest Sites, Agricultural And Forest Meteorology, 150(10), 1366-1372. https://doi.org/10.1016/j.agrformet.2010.06.007

CA-SF2: Saskatchewan - Western Boreal, forest burned in 1989

BADM for This Site

Access the Biological, Ancillary, Disturbance and Metadata (BADM) information and data for this site.

BADM contain information for many uses, such as characterizing a site’s vegetation and soil, describing disturbance history, and defining instrumentation for flux processing. They complement the flux/met data.

* Online updates are shown on the Overview tab real time. However, downloaded BADM files will not reflect those updates until they have been reviewed for QA/QC.

CA-SF2: Saskatchewan - Western Boreal, forest burned in 1989

Wind Roses

Click an image below to enlarge it, or use the navigation panel.
  • Image scale: 593m x 593m
  • Data Collected:
    • Wind roses use variables ‘WS’ and ‘WD’.
    Download Data Download Wind Rose as Image File (PNG)

    Wind Speed (m/s)

  • Graph Type
  • Wind Speed Scale
  • Wind Direction Scale (%)
  • Show Satellite Image
  • Show Wind Rose
    • Annual Average
    About Ameriflux Wind Roses
    Wind Rose Explanation
    A wind rose gives a succinct view of how wind speed and direction are typically distributed at a particular location. Presented in a circular format, a wind rose shows the frequency and intensity of winds blowing from particular directions. The length of each “spoke” around the circle indicates the amount of time (frequency) that the wind blows from a particular direction. Colors along the spokes indicate categories of wind speed (intensity). Each concentric circle represents a different frequency, emanating from zero at the center to increasing frequencies at the outer circles
    Utility
    This information can be useful to gain insight into regions surrounding a flux tower that contribute to the measured fluxes, and how those regions change in dependence of the time of day and season. The wind roses presented here are for four periods of the year, and in 16 cardinal directions. Graphics are available for all sites in the AmeriFlux network based on reported wind measurements at each site.
    Data from each site can be downloaded by clicking the ‘download’ button.
    Hover the cursor over a wind rose to obtain directions, speeds and intensities.
    Note that wind roses are not equivalent to flux footprints. Specifically, the term flux footprint describes an upwind area “seen” by the instruments measuring vertical turbulent fluxes, such that heat, water, gas and momentum transport generated in this area is registered by the instruments. Wind roses, on the other hand, identify only the direction and speed of wind.
    Where do these data come from?
    The wind roses are based on observed hourly data from the sites registered with the AmeriFlux Network.
    Parameters for AmeriFlux Wind Roses
    To use wind roses for a single AmeriFlux site, the following parameters may be most useful:
    • Wind Speed Scale: Per Site
    • Wind Direction Scale (%): Per Site
    To compare wind roses from more than one single AmeriFlux site, the following parameters may be most useful:
    • Wind Speed Scale: Non-Linear
    • Wind Direction Scale (%): AmeriFlux
    Mar - Jun; 6am - 6pm
    Mar - Jun; 6pm - 6am
    Jun - Sep; 6am - 6pm
    Jun - Sep; 6pm - 6am
    Sep - Dec; 6am - 6pm
    Sep - Dec; 6pm - 6am
    Dec - Mar; 6am - 6pm
    Dec - Mar; 6pm - 6am