Importance of calibration in determining forest stand transpiration using the thermal dissipation method
Importance of calibration in determining forest stand transpiration using the thermal dissipation method
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DOI:
10.1016/j.agrformet.2021.108356
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发表时间:
2021-05
影响因子:
6.2
通讯作者:
N. Fujime;T. Kumagai;T. Egusa;H. Momiyama;Y. Uchiyama
中科院分区:
文献类型:
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作者:
N. Fujime;T. Kumagai;T. Egusa;H. Momiyama;Y. Uchiyama
Forest transpiration (Tr) is the major hydrologic flux from terrestrial ecosystems; it dominates the catchment water budget and land surface energy balance and can be used as an index of exchange efficiency between vegetation and the atmosphere. The thermal dissipation method (TDM) is used to obtain the xylem sap flux density (Fd) of individual tree stems; it is among the most powerful tools for estimating forest standTr(Tr_stand) values. Individual treeTrvalues can be upscaled toTr_standas a product of stand total sapwood area (AS_stand) and stand meanFd(JS). In this study, we performed laboratory experiments using Japanese cedar (Cryptomeria japonicaD. Don) to examine errors inTr_standvalues generated by mis-estimation ofAS_standand/orJS. We found that simple color identification of the stem hydroactive zone in sapwood and heartwood had little effect on accurate estimation ofAS_standvalues. Then we examined the effects of mis-estimation ofJS, which is primarily the result ofFdmeasurement failures. Considering that uncertainties in heat-tracer-derivedFdvalues using the TDM have been identified in numerous previous studies, we applied calibration to improve the accuracy of TDM-Fdderivation using freshly cut sapwood segments of sample Japanese cedar stems and negative pressure as a driving force to determineFdwithin the segments experimentally. The calibration experiment revealed that the calibrated conversion equation for heat-tracer-derivedFdvalues resulted in values that differed significantly from those determined using the original TDM equation and significant underestimation ofTr_stand. TheFdcorrection increased the annualTr_standvalue from 229 to 593 mm year−1, while the corrected value was not significantly different from theTr_standvalue obtained from catchment-scale water budget observations. The novel TDM calibration equation improved TDM-basedTr_standestimates dramatically, highlighting the importance of this study's calibration method.