Modelling stemflow production by juvenile lodgepole pine (Pinus contorta var. latifolia) trees

Adam J. McKee , Darryl E. Carlyle-Moses

Journal of Forestry Research ›› 2016, Vol. 28 ›› Issue (3) : 565 -576.

PDF
Journal of Forestry Research ›› 2016, Vol. 28 ›› Issue (3) : 565 -576. DOI: 10.1007/s11676-016-0336-9
Original Paper

Modelling stemflow production by juvenile lodgepole pine (Pinus contorta var. latifolia) trees

Author information +
History +
PDF

Abstract

Stemflow is a focused point source input of precipitation and nutrients at the base of a tree or plant and can have a significant impact on site hydrology. To date, no known studies have modelled stemflow production for juvenile lodgepole pine (Pinus contorta var. latifolia). Meteorological conditions, tree characteristics, and stemflow were sampled for two juvenile lodgepole pine stands over the course of the 2009 growing season. Step-wise multiple regression was used to assess which meteorological and tree architecture variables influenced stemflow production for each research plot. Once predictor variables were identified, models were produced for each stand and a generic model was produced that applied to both plots. A model employing precipitation depth and crown projection area successfully explained 71.3% of the variation in stemflow production from sampled trees. Stemflow was found to represent 1.8% of the study period rainfall and, although not a large component of the plot-scale canopy water balance, it is an order of magnitude greater than the fractioning of stemflow from mature lodgepole and lodgepole pine dominated forest. Additionally, stemflow funnelling ratios were found to average 22.2 and 24.3 from the two sample plots over the study period with a single tree, single event maximum of 111.7 recorded for a tree with a 3.3 cm bole diameter and a rain depth of 17.4 mm.

Keywords

Lodgepole pine / Stemflow / Stemflow funnelling ratio

Cite this article

Download citation ▾
Adam J. McKee, Darryl E. Carlyle-Moses. Modelling stemflow production by juvenile lodgepole pine (Pinus contorta var. latifolia) trees. Journal of Forestry Research, 2016, 28(3): 565-576 DOI:10.1007/s11676-016-0336-9

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

Aboal JR, Morales D, Hernández JM, Jiménez MS. The measurement and modelling of the variation of stemflow in a laurel forest in Tenerife, Canary Islands. J Hydrol, 1999, 221(3): 161-175.

[2]

Bialkowski R, Buttle JM. Stemflow and throughfall contributions to soil water recharge under trees with differing branch architectures. Hydrol Process, 2015, 29(18): 4068-4082.

[3]

Brinson MM, Bradshaw HD, Holmes RN, Elkins JB Jr. Litterfall, stemflow, and throughfall nutrient fluxes in an alluvial swamp forest. Ecology, 1980, 61(4): 827-835.

[4]

British Columbia Ministry of Forests, Lands, and Natural Resource Operations (2015) Mountain Pine Beetle. Infestation Information. https://www.for.gov.bc.ca/hfp/mountain_pine_beetle/. Accessed May 2015

[5]

British Columbia Ministry of Water, Land and Air Protection (2004) Weather, Climate and the Future: BC’s Plan. http://www.env.gov.bc.ca/air/climate/index.html#1

[6]

Brown JH Jr, Barker AC Jr. An analysis of throughfall and stemflow in mixed oak stands. Water Resour Res, 1970, 6(1): 316-323.

[7]

Buttle JM, Toye HJ, Greenwood WJ, Bialkowski R. Stemflow and soil water recharge during rainfall in a red pine chronosequence on the Oak Ridges Moraine, southern Ontario, Canada. J Hydrol, 2014, 517: 777-790.

[8]

Cape JN, Brown AHF, Robertson SMC, Howson G, Paterson IS. Interspecies comparisons of throughfall and stemflow at three sites in northern Britain. For Ecol Manag, 1991, 46(3–4): 165-177.

[9]

Carlyle-Moses DE. A Reply to R. Keim’s Comment on ‘Measurement and modelling of growing-season canopy water fluxes in a mature mixed deciduous forest stand, southern Ontario, Canada. Agric For Meteorol, 2004, 124(3–4): 281-284.

[10]

Carlyle-Moses DE, Lishman CE. Throughfall heterogeneity and temporal persistence below and between the canopies of juvenile lodgepole pine (Pinus contorta). Hydrol Process, 2015, 29(18): 4051-4067.

[11]

Carlyle-Moses DE, Schooling JT. Tree traits and meteorological factors influencing the initiation and rate of stemflow from isolated deciduous trees. Hydrol Process, 2015, 29(18): 4083-4099.

[12]

Carlyle-Moses DE, Lishman CE, McKee AJ. A preliminary evaluation of throughfall sampling techniques in a mature coniferous forest. J For Res, 2014, 25(2): 407-413.

[13]

Chang S, Matzner E. The effect of beech stemflow on spatial patterns of soil solution chemistry and seepage fluxes in a mixed beech/oak stand. Hydrol Process, 2000, 14(1): 135-144.

[14]

Davie TJA, Durocher MG. A model to consider the spatial variability of rainfall partitioning within deciduous canopy. II. Model parameterization and testing. Hydrol Process, 1997, 11(11): 1525-1540.

[15]

Dombois MD, Ellenberg H. Aims and Methods of Vegetation Ecology, 1974, New York: John Wiley and Sons 67 92

[16]

Dunford EG, Neiderhof CH. Influence of aspen, young lodgepole pine, and open grassland types upon factors affecting water yield. J For, 1944, 42(9): 673-677.

[17]

Eaton B, Moore RD (2010) Regional Hydrology. In: Pike RG, Redding TE, Moore Rd, Winkler RD, Bladon KD (eds) Compendium of forest hydrology and geomorphology in British Columbia. Kamloops: Land management Handbook 66, BC Ministry of Forest and Range and FORREX Forum for Research and Extension in Natural Resources, p. 85–110

[18]

Ford ED, Deans JD. The effects of canopy structure on stemflow, throughfall and interception loss in a young sitka spruce plantation. J Appl Ecol, 1978, 15(3): 905-917.

[19]

Hanchi A, Rapp M. Stemflow determination in forest stands. For Ecol Manag, 1997, 97(3): 231-235.

[20]

Herwitz SR. Infiltration-excess caused by stemflow in a cyclone-prone tropical rainforest. Earth Surf Proc Land, 1986, 11(4): 401-412.

[21]

Herwitz SR. Raindrop impact and water flow on the vegetative surfaces of trees and the effects on stemflow and throughfall generation. Earth Surf Proc Land, 1987, 12(4): 425-432.

[22]

Johnson MS, Lehmann J. Double-funnelling of trees: stemflow and root-induced preferential flow. Ecoscience, 2006, 13(3): 324-333.

[23]

Levia DF. Differential winter stemflow generation under contrasting storm conditions in a southern New England broad-leaved deciduous forest. Hydrol Process, 2004, 18(6): 1105-1112.

[24]

Levia DF, Frost EE. A review and evaluation of stemflow literature in the hydrologic and biogeochemical cycles of forest and agricultural ecosystems. J Hydrol, 2003, 274(1–4): 1-29.

[25]

Levia DF, Germer S. A review of stemflow generation dynamics and stemflow-environment interactions in forests and shrublands. Rev Geophys, 2015, 53(3): 673-714.

[26]

Levia DF, Keim RF, DE Carlyle-Moses, Frost EE. Levia DF, DE Carlyle-Moses, Tanaka T. Throughfall and stemflow in wooded ecosystems. Forest hydrology and biogeochemistry: synthesis of past research and future directions, 2011 216 Germany: Springer 425 444

[27]

Levia DF, Michalzik B, Näthe K, Bischoff S, Richter S, Legates DR. Differential stemflow yield from European beech saplings: the role of individual canopy structure metrics. Hydrol Process, 2015, 29: 43-51.

[28]

Manfroi OJ, Koichiro K, Nobuaki T, Masakazu S, Nakagawa M, Nakashizuka T, Chong L. The stemflow of trees in a Bornean lowland tropical forest. Hydrol Process, 2004, 18(13): 2455-2474.

[29]

Martínez-Meza E, Whitford WG. Stemflow, throughfall and channelization of stemflow by roots in three Chihuahuan desert shrubs. J Arid Environ, 1996, 32(3): 271-287.

[30]

McKee AJ, Carlyle-Moses DE. Stemflow: a potentially important point source of water for growth. Link Innov Netw Knowl, 2010, 11(2): 11-12.

[31]

Moore RD, Winkler R, Carlyle-Moses D, Spittlehouse D, Giles T, Phillips J, Leach J, Eaton B, Owens P, Petticrew E, Blake W, Heise B, Redding T. Watershed response to the McLure forest fire: presentation summaries from the Fishtrap Creek workshop. Streamline Watershed Manag Bull, 2008, 12(1): 1-11.

[32]

Murakami S. Abrupt change in annual stemflow with growth in a young stand of Japanese cypress. Hydrol Res Lett, 2009, 3: 32-35.

[33]

Návar J. The causes of stemflow variation in three semi-arid growing species of northeastern Mexico. J Hydrol, 1993, 145(1–2): 175-190.

[34]

Návar J. Stemflow variation in Mexico’s northeastern forest communities: its contribution to soil moisture content and aquifer recharge. J Hydrol, 2011, 408(1–2): 35-42.

[35]

Park H, Hattori S. Applicability of stand structural characteristics to stemflow modelling. J For Res, 2002, 7(2): 91-98.

[36]

Piñeiro G, Perelman S, Guerschman JP, Paruelo JM. How to evaluated models: observed vs. predicted or predicted vs. observed?. Ecol Model, 2008, 216(3–4): 316-322.

[37]

Schooling JT, Carlyle-Moses DE. The influence of rainfall depth class and deciduous tree traits on stemflow production in an urban park. Urban Ecosyst, 2015, 18(4): 1261-1284.

[38]

Schroth G, Elias MEA, Uguen K, Seixas R, Zech W. Nutrient fluxes in rainfall, throughfall and stemflow in tree-based land use systems and spontaneous tree vegetation of central Amazonia. Agric Ecosyst Environ, 2001, 87(1): 37-49.

[39]

Spittlehouse D (1998) Rainfall interception in young and mature conifer forests in British Columbia. Proceedings 23rd conference on agricultural and forest meteorology, boston: american meteorological society, p.40–44

[40]

Tanaka T, Taniguchi M, Tsujimura M. Significance of stemflow in groundwater recharge. 2: a cylindrical infiltration model for evaluating the stemflow contribution to groundwater recharge. Hydrol Process, 1996, 10(1): 81-88.

[41]

Taniguchi M, Tsujimura M, Tanaka T. Significance of stemflow in groundwater recharge. 1: evaluation of this stemflow contribution to recharge using a mass balance approach. Hydrol Process, 1996, 10(1): 71-80.

[42]

United States Environmental Protection Agency. Meteorological monitoring guidance for regulatory modeling applications, 2000, Triangle Park: Office of Air Quality Planning and Standards Research 1 177

[43]

Van Stan JT II, Levia DF. Inter- and intraspecific variation of stemflow production from Fagus grandifolia Ehrh. (American beech) and Liriodendron tulipifera L. (yellow poplar) in relation to bark microrelief in the eastern United States. Ecohydrology, 2010, 3(1): 11-19.

[44]

Van Stan JT II, Van Stan JH, Levia DF. Meteorological influences on stemflow generation across diameter size classes of two morphologically distinct deciduous species. Biometeorology, 2014, 58(10): 2059-2069.

[45]

Voigt GK. Distribution of rainfall under forest stands. For Sci, 1960, 6(1): 2-10.

[46]

Wang XP, Wang ZN, Berndtsson R, Zhang YF, Pan YX. Desert shrub stemflow and its significance in soil moisture replenishment. Hydrol Earth Syst Process, 2011, 15: 561-567.

[47]

Whitford WH, Anderson J, Rice PM. Stemflow contribution to the ‘fertile island’ effect in creosotebush, Larrea tridentate. J Arid Environ, 1997, 35(3): 451-457.

[48]

Winkler RD, Spittlehouse DL, Golding DL. Measured differences in snow accumulation and melt among clearcut, juvenile, and mature forests in southern British Columbia. Hydrol Process, 2005, 19(1): 51-62.

AI Summary AI Mindmap
PDF

136

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/