Skip to main content
Log in

Surface energy fluxes and control of evapotranspiration from a Carex lasiocarpa mire in the Sanjiang Plain, Northeast China

  • Original Paper
  • Published:
International Journal of Biometeorology Aims and scope Submit manuscript

Abstract

Data from four components of the radiation balance were used to investigate the surface energy budgets for a Carex lasiocarpa mire in the Sanjiang Plain, Northeast China, and the controlling factors of the evapotranspiration (ET) were discussed in detail. During the growing season 2006, the shortwave radiation (SW↓) reaching the mire surface added up to 2,854.3 MJ m−2 and the net radiation (Rn) was 1,637.4 MJ m−2 in total, with an average of 9.86 MJ m−2 day−1. G was the smallest flux at the water-atmosphere interface, with an average of about 0.91 MJ m−2 day−1, but showed high relative variability, even changing its sign. The latent and sensible heat fluxes (LE and H) amounted to 787.48 and 476.26 MJ m−2, respectively, and the total sum of LE and H accounted for 77.18% of Rn. By conversion from LE, the average value of ET from the mire was 1.84 mm day−1, amounting to 298.8 mm. The total ET was almost 60% of the total rainfall in the same period, proving that ET is the primary water consumer in the mire. The growth of C. lasiocarpa was related closely with surface resistance (r s), and analysis of partial correlation indicated that r s correlated negatively with leaf area index (LAI) when the interference of the available energy, Rn-G, was removed. There was a strong linkage between r s and the evaporative fraction [LE/(LE + H)] as well as Bowen ratio (β). r s was the key factor in controlling the variation of ET and regulating energy partitioning between LE and H. During the whole growing season, r s and R nG were the two main factors coupled in ET processes. In spring, r s dominated ET processes, and the increase in LAI led to a decrease in r s, which in turn accelerated ET as vegetation developed until late August. After August, the available energy controlled the process of ET completely until ET reached an equilibrium in mid-October.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Subscribe and save

Springer+ Basic
$34.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or eBook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13
Fig. 14

Similar content being viewed by others

Explore related subjects

Discover the latest articles and news from researchers in related subjects, suggested using machine learning.

References

  • Acreman MC, Harding RJ, Lloyd CR, McNeil DD (2003) Evaporation characteristics of wetlands: experience from a wet grassland and a reedbed using eddy correlation measurements. Hydrol Earth Syst Sci 7:11–21

    Article  Google Scholar 

  • Admiral SW, Lafleur PM, Roulet NT (2006) Controls on latent heat flux and energy partitioning at a peat bog in eastern Canada. Agric For Meteorol 140:308–321

    Article  Google Scholar 

  • Blanken PD, Rouse WR (1996) Evidence of water conservation mechanisms in several subarctic wetland species. J Appl Ecol 33:842–850

    Article  Google Scholar 

  • Bubier J, Moore T (1994) An ecological perspective on methane emissions from northern wetlands. Trends Ecol Evol 9:460–464

    Article  CAS  Google Scholar 

  • Comer NT, Lafeur PM, Roulet NT, Letts MG, Skarupa M, Verseghy D (2000) A test of the Canadian Land Surface Scheme (CLASS) for a variety of wetland types. Atmos Ocean 38:161–179

    Article  Google Scholar 

  • Deng W, Luan ZQ, Hu JM, Yan MH (2005) Study on water flux in the typical wetlands in the Sanjing Plain (in Chinese). Wetlands Science 3(1):32–36

    Google Scholar 

  • Drexler JZ, Snyder RL, Spano D, Paw UKT (2004) A review of models and micrometeorological method used to estimate wetland evapotranspiration. Hydrol Process 18:2071–2101

    Article  Google Scholar 

  • Eugster W, Rouse WR, Pielke RA, McFadden JP, Baldocchi DD, Kittel TGF, Chapin FS, Liston GE, Vidale PL, Vaganov E, Chambers S (2000) Land-atmosphere energy exchange in Arctic tundra and boreal forest: available data and feedbacks to climate. Glob Chang Biol 6:84–115

    Article  Google Scholar 

  • Finnigan JJ, Raupach MR (1987) Transfer processes in plant canopies in relation to stomatal characteristics. In: Zeiger E, Farquar GD, Cowan IR (eds) Stomatal function. Stanford University Press, Stanford, pp 385–429

    Google Scholar 

  • Goulden ML, Litvak M, Miller SD (2007) Factors that control Typha marsh evapotranspiration. Aquat Bot 86:97–106

    Article  Google Scholar 

  • Guo YD (2008) Influence of Carex lasiocarpa vegetation on the evapotranspiration of mire in the Sanjiang Plain (in Chinese). Wetland Sci 6(6):392–397

    Google Scholar 

  • He CQ, Li L, Guo C, Lu XY (2003) The utilization and distribution of the sunlight radiation energy in Carex lasiocarpa wetland in Sanjiang Plain (in Chinese). Acta Hydrobiol Sin 27(5):502–506

    Google Scholar 

  • Jackson GE, Irvine J, Grace J (1999) Xylem acoustic emissions and water relations of Calluna vulgaris L. at two climatological regions of Britain. Plant Ecol 140:3–14

    Article  Google Scholar 

  • Kelliher FM, Leuning R, Raupach MR, Schulze ED (1995) Maximum conductances for evaporation from global vegetation types. Agric For Meteorol 73:1–16

    Article  Google Scholar 

  • Kellner E (2001) Surface energy fluxes and control of evapotranspiration from a Swedish Sphagnum mire. Agric For Meteorol 110:101–123

    Article  Google Scholar 

  • Kellner E, Halldin S (2002) Water budget and surface-layer water storage in a Sphagnum bog in central Sweden. Hydrol Process 16(1):87–103

    Article  Google Scholar 

  • Kim J, Verma SB (1996) Surface exchange of water vapour between an open Sphagnum fen and the atmosphere. Boundary Layer Meteorol 79:243–264

    Article  Google Scholar 

  • Lafleur PM (1988) Leaf conductance of four species growing in a subarctic marsh. Can J Bot 66:1367–1375

    Article  Google Scholar 

  • Lafleur PM, McCaughey JH, Joiner DW, Bartlett PA, Jelinski DE (1997) Seasonal trends in energy, water, and carbon dioxide fluxes at a northern boreal wetland. J Geophys Res Atmos 102:29009–29020

    Article  CAS  Google Scholar 

  • Li Z, Yu G, Wen X, Zhang L, Ren C, Fu Y (2004) The evaluation of energy closure status of China FLUX (in Chinese). Sci China Ser D Earth Sci 34:46–56

    Google Scholar 

  • Li YN, Zhao L, Zhou HK, Xu SX, Zhang FW (2007) Changes in reflected radiation and reflectivity for growing season of alpine swamp in the northern Qinghai (in Chinese). J Glaciol Geocryol 29(1):137–143

    Google Scholar 

  • Lovelli S, Perniola M, Arcieri M, Rivelli AR, Di Tommaso T (2008) Water use assessment in muskmelon by the Penman-Monteith “one-step” approach. Agric Water Manag 95(10):1153–1160

    Article  Google Scholar 

  • Molder M, Kellner E (2001) Excess resistance of bog surfaces in central Sweden. Agric For Meteorol 112:23–30

    Article  Google Scholar 

  • Moore KE, Fitzjarrald DR, Wofsy SC, Daube BC, Munger JW, Bakwin PS, Crill P (1994) A season of heat, water vapor, total hydrocarbon, and ozone fluxes at a sub-arctic fen. J Geophys Res Atmos 99:1937–1952

    Article  CAS  Google Scholar 

  • Penman HL (1948) Natural evaporation from open water, bare soil and grass. Proc R Soc Lond A 193:120–145

    Article  CAS  Google Scholar 

  • Priban K, Ondok JP (1985) Heat balance components and evapotranspiration from a sedge-grass marsh. Folia Geobot Phytotaxon 20:41–56

    Google Scholar 

  • Price JS (1994) Evapotranspiration from a lakeshore Typha marsh on Lake Ontario. Aquat Bot 48:261–272

    Article  Google Scholar 

  • Song KS, Liu DW, Wang ZM (2008) Land use change in Sanjiang Plain and its driving forces analysis since 1954. Acta Geogr Sin 63(1):93–104

    Google Scholar 

  • Stigter CJ (1980) Assessment of the quality of generalized wind functions in Penman’s equations. J Hydrol 45:321–331

    Article  Google Scholar 

  • Sun L, Song CC (2008) Evapotranspiration from freshwater marsh in the Sanjiang Plain, Northeast China. J Hydrol 352:202–210

    Article  Google Scholar 

  • Takagi K, Tsuboya T, Takahashi H (1998) Diurnal hysteresis of stomatal and bulk surface conductances in relation to vapor pressure deficit in a cool-temperature wetland. Agric For Meteorol 91:177–191

    Article  Google Scholar 

  • Tanaka K, Tamagawa I, Ishikawa H, MaY HuZ (2003) Surface energy budget and closure of the eastern Tibetan Plateau during the GAME-TibetIOP 1998. J Hydrol 283:169–183

    Article  Google Scholar 

  • Webb EK, Pearman GI, Leuning R (1980) Correction of flux measurements for density effects due to heat and water vapor transfer. Q J R Meteorol Soc 106:85–100

    Article  Google Scholar 

  • Wessel DA, Rouse WR (1994) Modelling evaporation from wetland tundra. Boundary-Layer Meteorol 68:109–130

    Article  Google Scholar 

Download references

Acknowledgments

The work was funded by Major Project of Chinese National Programs for Fundamental Research and Development (2009CB421103, 2010CB951304), Knowledge Innovation Program of Chinese Academy of Sciences (KZCX2-YW-309; KZCX2-YW-Q06-03), and Youth Doctor Foundation of Northeast Institute of Geography and Agroecology (08H2081).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Yuedong Guo.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Guo, Y., Sun, L. Surface energy fluxes and control of evapotranspiration from a Carex lasiocarpa mire in the Sanjiang Plain, Northeast China. Int J Biometeorol 56, 221–232 (2012). https://doi.org/10.1007/s00484-011-0415-8

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00484-011-0415-8

Keywords