کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6537834 158344 2013 11 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
High sensitivity of peat moisture content to seasonal climate in a cutaway peatland cultivated with a perennial crop (Phalaris arundinaceae, L.): A modeling study
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات علم هواشناسی
پیش نمایش صفحه اول مقاله
High sensitivity of peat moisture content to seasonal climate in a cutaway peatland cultivated with a perennial crop (Phalaris arundinaceae, L.): A modeling study
چکیده انگلیسی
In this study, a process-based model was developed for studying the climatic sensitivity of the soil moisture content (θ) in a cutaway peatland cultivated with a perennial crop (Phalaris arundinaceae, L., RCG). The model was parameterized based on the canopy development and the soil properties measured in Linnansuo peatland in Eastern Finland. The model was also calibrated and validated by continuous measurements of meteorology, soil temperature, soil moisture and energy fluxes (eddy covariance system) during a wet year (2009) and a dry year (2010). The results showed that the model captured well the seasonal trend of the latent heat flux during the two-year period. Moreover, the model explained the major seasonal variations of the moisture content in multiple peat layers in the soil profile. Sensitivity analysis of the model showed that the fluctuation of the water table (WT) had little impact on the seasonal dynamics of the peat moisture content in the Linnansuo site. These results indicated that anthropological disturbances, such as peat extraction, drainage and energy crop cultivation, critically weakened the θ-WT interaction in the Linnansuo peatland. Moreover, these changes indicated the high climatic sensitivity of the peat moisture content especially to the variations of the seasonal pattern of precipitation.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Agricultural and Forest Meteorology - Volume 180, 15 October 2013, Pages 225-235
نویسندگان
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