On the spectrum of soil moisture in a shallow-rooted uniform pine forest: from hourly to inter-annual scales

dc.contributor.authorKatul, Gabriel G.
dc.contributor.authorPorporato, Amilcare
dc.contributor.authorDaly, Edoardo
dc.contributor.authorOishi, A. Christopher
dc.contributor.authorKim, Hyun-Seok
dc.contributor.authorStoy, Paul C.
dc.contributor.authorJuang, Jehn-Yih
dc.contributor.authorSiqueira, Mario B. S.
dc.date.accessioned2018-10-29T21:49:08Z
dc.date.available2018-10-29T21:49:08Z
dc.date.issued2007-05
dc.description.abstractThe spectrum of soil moisture content at scales ranging from 1 hour to 8 years is analyzed for a site whose hydrologic balance is primarily governed by precipitation (p), and evapotranspiration (ET). The site is a uniformly planted loblolly pine stand situated in the southeastern United States and is characterized by a shallow rooting depth (RL) and a near‐impervious clay pan just below RL. In this setup, when ET linearly increases with increasing root zone soil moisture content (θ), an analytical model can be derived for the soil moisture content energy spectrum (Es(f), where f is frequency) that predicts the soil moisture “memory” (taken as the integral timescale) as β1−1 ≈ ηRL/ETmax, where ETmax is the maximum measured hourly ET and η is the soil porosity. The spectral model suggests that Es(f) decays at f−2−α at high f but almost white (i.e., f0) at low f, where α is the power law exponent of the rainfall spectrum at high f (α ≈ 0.75 for this site). The rapid Es(f) decay at high f makes the soil moisture variance highly imbalanced in the Fourier domain, thereby permitting much of the soil moisture variability to be described by a limited number of Fourier modes. For the 8‐year data collected here, 99.6% of the soil moisture variance could be described by less than 0.4% of its Fourier modes. A practical outcome of this energy imbalance in the frequency domain is that the diurnal cycle in ET can be ignored if β1−1 (estimated at 7.6 days from the model) is much larger than 12 hours. The model, however, underestimates the measured Es(f) at very low frequencies (f ≪ β1) and its memory, estimated from the data at 42 days. This underestimation is due to seasonality in ETmax and to a partial decoupling between ET and soil moisture at low frequencies.en_US
dc.identifier.citationKatul, Gabriel G., Porporato, Amilcare, Daly, Edoardo, Oishi, A. Christopher, Kim, Hyun-Seok, Stoy, Paul C., Juang, Jehn-Yih, Siqueira, Mario B. S. (2007) On the spectrum of soil moisture in a shallow-rooted uniform pine forest: from hourly to inter-annual scales. Water Resources Research 43: W05428. DOI: 10.1029/2006WR005356.en_US
dc.identifier.issn1944-7973
dc.identifier.urihttps://scholarworks.montana.edu/handle/1/14961
dc.language.isoenen_US
dc.rightsThis Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).en_US
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en_US
dc.titleOn the spectrum of soil moisture in a shallow-rooted uniform pine forest: from hourly to inter-annual scalesen_US
dc.typeArticleen_US
mus.citation.issue5en_US
mus.citation.journaltitleWater Resources Researchen_US
mus.citation.volume43en_US
mus.data.thumbpage6en_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doi10.1029/2006WR005356en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.departmentLand Resources & Environmental Sciences.en_US
mus.relation.universityMontana State University - Bozemanen_US

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