Simulation of Land-Atmosphere Water and Heat Exchange over the Underlying Surface of Different Crops on the Loess Plateau
Received date: 2022-03-30
Revised date: 2022-08-15
Online published: 2024-03-27
Changes in the planting structure of farmland on the Loess Plateau impact land surface energy and water exchange, regional evapotranspiration, etc.The complex hydrothermal coupling mechanism of different crop underlying surfaces plays an essential role in the land-atmosphere interaction on the Loess Plateau.In this paper, based on the observation data of 34 months from 2019 to 2021 in the east of Gansu province, combined with CLM5.0-BGCCROP coupled with the crop module, the land surface characteristics of different typical crops (winter wheat, corn, and apple forest) on the Loess Plateau were offline single-point simulated.To verify the simulation ability of CLM5.0 on the land surface processes of agricultural fields on the Loess Plateau and compare the differences in soil temperature, soil liquid water content, and surface energy fluxes of different crops.The results showed that: (1) CLM5.0 has a better simulation effect on soil temperature and liquid water content characteristics, average RMSE is less than 2.5 and 0.1 m3·m-3, respectively.The simulated soil temperature values in the wheat field are high, and there is a cold bias in the corn and apple fields.Winter wheat, which has a dry growth period, caused more soil drying than corn.Apple forest, which has a rich root system, absorbed more soil water, making the soil drier overall.(2) Part of the simulation bias is due to setting crop underlying surfaces to a single crop functional type in the model, overestimating the leaf area index of crops during the growth period, underestimating the surface albedo, overestimating the net radiation flux, and converting more energy flux into sensible and latent heat flux.(3) Another part of the simulation bias comes from the diverse crop management methods in the farmland.For example, crop fields are not completely tilled to bare soil after harvest, and the model overestimates soil temperature and soil liquid water content in wheat and corn fields.The model does not have the mulching option, which leads to the low simulated soil temperature and soil liquid water content in corn fields, about 1.84 and 0.058 m3·m-3, respectively.(4) The winter wheat and corn mixed crop underlying surface simulation experiment could better simulate the surface energy fluxes, and the simulated average deviations of net radiation, sensible heat flux, and latent heat flux were -6.13 W·m-2, 11.46 W·m-2, -1.97 W·m-2, respectively.During the growth period, canopy transpiration dominates, and with the increase of crop leaf area index, sensible heat flux decreases, soil temperature decreases, latent heat flux increases, and soil liquid water content decreases.
Wei JIN , Yinhuan AO , Xiaohang WEN , Zhaoguo LI , Xianhong MENG , Jianglin LI , Gang ZHAO , Mingshan DENG , Lijun XIE , Zihang CHEN . Simulation of Land-Atmosphere Water and Heat Exchange over the Underlying Surface of Different Crops on the Loess Plateau[J]. Plateau Meteorology, 2023 , 42(3) : 671 -686 . DOI: 10.7522/j.issn.1000-0534.2022.00078
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | |
null | 陈紫薇, 2021.覆膜对小麦-玉米轮作系统土壤水热、 作物生长和产量的影响[D].咸阳: 西北农林科技大学, DOI: 10.27409/d.cnki.gxbnu.2021.000605 . |
null | |
null | 李得勤, 张述文, 文小航, 等, 2016.土壤湿度参数化及对天气和气候模拟影响的研究进展[J].地球科学进展, 31(3): 236-247.DOI: 10.11867/j.issn.1001-8166.2016.03.236 . |
null | 李时越, 杨凯, 王澄海, 2018.陆面模式CLM4.5在青藏高原土壤冻融期的偏差特征及其原因[J].冰川冻土, 40(2): 322-334.DOI: 10.7522/j.issn.1000-0240.2018.0037 . |
null | 陆军胜, 2021.滴灌水肥一体化冬小麦/夏玉米水氮效应及夏玉米氮肥供应决策研究[D].咸阳: 西北农林科技大学, DOI: 10. 27409/d.cnki.gxbnu.2021.001906 . |
null | 邵进, 2019.黄土塬区深层土壤水文过程及其变化规律研究[D].咸阳: 西北农林科技大学.DOI: 10.27409/d.cnki.gxbnu. 2019.000045 . |
null | 孙昊蔚, 2020.气候变化下黄土高原作物产量与土壤水分模拟[D].咸阳: 西北农林科技大学, DOI: 10.27409/d.cnki.gxbnu. 2020.000933 . |
null | 王澄海, 杨凯, 张飞民, 等, 2021.青藏高原土壤冻融过程的气候效应: 进展和展望[J].高原气象, 40(6): 1318-1336.DOI: 10. 7522/j.issn.1000-0534.2021.zk021 . |
null | 王丹云, 吕世华, 韩博, 等, 2018.黄土高原春季植被变化分布与变化特征及其对春旱的响应研究[J].高原气象, 37(5): 1208-1219.DOI: 10.7522/j.issn.1000-0534.2018.00033 . |
null | 王菲, 陈报章, 陈婧, 等, 2022.华北平原冬小麦——夏玉米轮作区DLM与CLM5模型模拟对比研究[J].地理科学进展, 41(2): 289-303.DOI: 10.18306/dlkxjz.2022.02.009 . |
null | 王龙欢, 谢正辉, 贾炳浩, 等, 2021.陆面过程模式研究进展——以CAS-LSM为例[J].高原气象, 40(6): 1347-1363.DOI: 10. 7522/j.issn.1000-0534.2021.zk016 . |
null | 王宇轩, 奥银焕, 李照国, 等, 2021.黑河中下游不同类型下垫面的能量收支差异及其成因研究[J].高原气象, 40(3): 495-509.DOI: 10.7522/j.issn.1000-0534.2020.00100 . |
null | 吴笛, 胡泽勇, 付春伟, 等, 2022.基于CLM4.5的高寒草地辐射收支和水热交换的数值模拟研究[J].高原气象, 41(1): 107-121.DOI: 10.7522/j.issn.1000-0534.2021.00045 . |
null | 张宝庆, 邵蕊, 赵西宁, 等, 2020.大规模植被恢复对黄土高原生态水文过程的影响[J].应用基础与工程科学学报, 28(3): 594-606.DOI: 10.16058/j.issn.1005-0930.2020.03.008 . |
null | 张宝庆, 田磊, 赵西宁, 等, 2021.植被恢复对黄土高原局地降水的反馈效应研究[J].中国科学: 地球科学, 51(7): 1080-1091.DOI: 10.1360/SSTe-2020-0273 . |
null |
/
〈 |
|
〉 |