Can complementary relationship models estimate actual evapotranspiration during soil freeze-thaw cycles?

Measured daily evapotranspiration during soil freeze-thaw cycles by two lysimeters, with the size of 40 cm in depth and 31.5 cm in diameter. Estimated daily evapotranspiration during soil freeze-thaw cycles by five complementary relationship models, advection-aridity (AA) model of Brutsaert and Stricker, the GG model proposed by Granger and Gray, Morton’s complementary relationship areal evapotranspiration (CRAE) model, the Han model, and Brutsaert model.

本数据集涵盖两类数据：一是采用两台规格为深度40 cm、直径31.5 cm的蒸渗仪（lysimeter）实测得到的土壤冻融循环期间的日蒸散发量；二是基于5种互补关系模型估算得到的同期土壤冻融循环期间的日蒸散发量，这5种模型分别为布鲁特萨尔特与施特里克提出的平流-干旱（AA）模型、格兰杰与格雷提出的GG模型、莫顿的区域蒸散发互补关系（CRAE）模型、韩模型以及布鲁特萨尔特模型。