CA-Ca2: British Columbia - Clearcut Douglas-fir stand (harvested winter 1999/2000)
| Tower_team: | |
| PI: | T. Andrew Black andrew.black@ubc.ca - University of British Columbia, Vancouver |
| Lat, Long: | 49.8705, -125.2909 |
| Elevation(m): | 300 |
| 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: | Cfb (Marine West Coast: mild with no dry season, warm summer) |
| Mean Annual Temp (Ā°C): | 9.86 |
| Mean Annual Precip. (mm): | 1474 |
| Flux Species Measured: | CO2 |
| Years Data Collected: | 2000 - Present |
| Years Data Available: | AmeriFlux BASE 1999 - 2010 Data Citation |
| Data Use Policy: | AmeriFlux CC-BY-4.0 Policy1 |
| Description: | |
| URL: | http://www.fluxnet-canada.ca/ |
| Research Topics: | — |
| Acknowledgment: | — |
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CA-Ca2: British Columbia - Clearcut Douglas-fir stand (harvested winter 1999/2000)
Use the information below for citation of this site. See the Data Policy page for more details.
DOI(s) for citing CA-Ca2 data
Data Use Policy: AmeriFlux CC-BY-4.0 License
This siteās data can also be used under the more restrictive AmeriFlux Legacy Policy.
The AmeriFlux Legacy Policy must be followed if CA-Ca2 data are combined with data from sites that require the AmeriFlux Legacy Policy.
- AmeriFlux BASE: https://doi.org/10.17190/AMF/1480301
Citation: T. Andrew Black (2018), AmeriFlux BASE CA-Ca2 British Columbia - Clearcut Douglas-fir stand (harvested winter 1999/2000), Ver. 1-5, AmeriFlux AMP, (Dataset). https://doi.org/10.17190/AMF/1480301
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Publication(s) for citing site characterization
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CA-Ca2: British Columbia - Clearcut Douglas-fir stand (harvested winter 1999/2000)
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CA-Ca2: British Columbia - Clearcut Douglas-fir stand (harvested winter 1999/2000)
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CA-Ca2: British Columbia - Clearcut Douglas-fir stand (harvested winter 1999/2000)
MODIS NDVI
The time series shows the 16-day Normalized Difference Vegetation Index (NDVI) average from the MOD13Q1 data product.
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For other related products, visit MODIS/VIIRS Fixed Sites Subsets Tool.
Citation:
ORNL DAAC. 2018. MODIS and VIIRS Land Products Fixed Sites Subsetting and Visualization Tool. ORNL DAAC, Oak Ridge, Tennessee, USA. https://doi.org/10.3334/ORNLDAAC/1567
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CA-Ca2: British Columbia - Clearcut Douglas-fir stand (harvested winter 1999/2000)
Search Publications for this Site
Publications Found: 10
| AmeriFlux Publications | Add Publication |
| 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-Haƫntjens, 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 |
| 2013 | Barr, A., Richardson, A., Hollinger, D., Papale, D., Arain, M., Black, T., Bohrer, G., Dragoni, D., Fischer, M., Gu, L., Law, B., Margolis, H., McCaughey, J., Munger, J., Oechel, W., Schaeffer, K. (2013) Use Of Change-Point Detection For FrictionāVelocity Threshold Evaluation In Eddy-Covariance Studies, Agricultural And Forest Meteorology, 171-172, 31-45. https://doi.org/10.1016/j.agrformet.2012.11.023 |
| 2009 | Krishnan, P., Black, T. A., Jassal, R. S., Chen, B., Nesic, Z. (2009) Interannual Variability Of The Carbon Balance Of Three Different-Aged Douglas-Fir Stands In The Pacific Northwest, Journal Of Geophysical Research, 114(G4), . https://doi.org/doi:10.1029/2008JG000912 |
| 2018 | Chu, H., Baldocchi, D. D., Poindexter, C., Abraha, M., Desai, A. R., Bohrer, G., Arain, M. A., Griffis, T., Blanken, P. D., O'Halloran, T. L., Thomas, R. Q., Zhang, Q., Burns, S. P., Frank, J. M., Christian, D., Brown, S., Black, T. A., Gough, C. M., Law, B. E., Lee, X., Chen, J., Reed, D. E., Massman, W. J., Clark, K., Hatfield, J., Prueger, J., Bracho, R., Baker, J. M., Martin, T. A. (2018) Temporal Dynamics Of Aerodynamic Canopy Height Derived From Eddy Covariance Momentum Flux Data Across North American Flux Networks, Geophysical Research Letters, 45, 9275ā9287. https://doi.org/10.1029/2018GL079306 |
| 2015 | Dennis Baldocchi, Cove Sturtevant (2015) Does day and night sampling reduce spurious correlation between canopy photosynthesis and ecosystem respiration?, Agricultural and Forest Meteorology, 207, 117-126. https://doi.org/10.1016/j.agrformet.2015.03.010 |
| 2006 | Coursolle, C., Margolis, H. A., Barr, A. G., Black, T. A., Amiro, B. D., McCaughey, J. H., Flanagan, L. B., Lafleur, P. M., Roulet, N. T., Bourque, C. P., Arain, M. A., Wofsy, S. C., Dunn, A., Morgenstern, K., Orchansky, A. L., Bernier, P. Y., Chen, J. M., Kidston, J., Saigusa, N., Hedstrom, N. (2006) Late-Summer Carbon Fluxes From Canadian Forests And Peatlands Along An East-ĀWest Continental Transect, Canadian Journal Of Forest Research, 36(3), 783-800. https://doi.org/10.1139/x05-270 |
| 2006 | Humphreys, E. R., Black, T. A., Morgenstern, K., Cai, T., Drewitt, G. B., Nesic, Z., Trofymow, J. (2006) Carbon Dioxide Fluxes In Coastal Douglas-Fir Stands At Different Stages Of Development After Clearcut Harvesting, Agricultural And Forest Meteorology, 140(1-4), 6-22. https://doi.org/10.1016/j.agrformet.2006.03.018 |
| 2006 | Chen, J. M., Govind, A., Sonnentag, O., Zhang, Y., Barr, A., Amiro, B. (2006) Leaf Area Index Measurements At Fluxnet-Canada Forest Sites, Agricultural And Forest Meteorology, 140(1-4), 257-268. https://doi.org/10.1016/j.agrformet.2006.08.005 |
| 2008 | Jassal, R. S., Black, T. A., Novak, M. D., Gaumont-Guay, D., Nesic, Z. (2008) Effect Of Soil Water Stress On Soil Respiration And Its Temperature Sensitivity In An 18-Year-Old Temperate Douglas-Fir Stand, Global Change Biology, 14(6), 1305-1318. https://doi.org/10.1111/j.1365-2486.2008.01573.x |
CA-Ca2: British Columbia - Clearcut Douglas-fir stand (harvested winter 1999/2000)
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CA-Ca2: British Columbia - Clearcut Douglas-fir stand (harvested winter 1999/2000)
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AĀ wind roseĀ 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
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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.
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The wind roses are based on observed hourly data from the sites registered with the AmeriFlux Network.
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