植物生态学报 ›› 2013, Vol. 37 ›› Issue (6): 492-502.DOI: 10.3724/SP.J.1258.2013.00051
收稿日期:
2013-01-09
接受日期:
2013-03-27
出版日期:
2013-01-09
发布日期:
2013-06-05
通讯作者:
孙鹏森
基金资助:
LIU Ning1,SUN Peng-Sen1,*(),LIU Shi-Rong1,SUN Ge2
Received:
2013-01-09
Accepted:
2013-03-27
Online:
2013-01-09
Published:
2013-06-05
Contact:
SUN Peng-Sen
摘要:
在复杂的气候变化条件下, 利用水碳耦合模型进行生态水文学研究成为主要的研究手段和途径。该文以杂谷脑河上游流域为例, 在确定生态水文模型WaSSI-C模拟尺度的基础上, 探讨水碳耦合模型在中国西南湿润地区的适用性。杂古脑河上游流域位于岷江上游, 隶属于长江流域。在分析和讨论了模型结构和机理的基础上, 分别对模型蒸散和融雪计算进行了补充改进, 以提高模型的适用性。将1988-1996年作为模型的率定期, 1997-2006年作为模型的验证期, 分别在率定期和验证期利用实测的径流数据和中分辨率成像光谱仪数据的总初级生产力、蒸散(ET)数据, 对模拟结果进行对比验证。并利用决定系数(R2)和Nash-Sutcliffe效率系数(NS)两个指标对模拟效果进行评价。流域总径流率定期和验证期对比验证的R2分别为0.86和0.78; NS分别为0.82和0.67。总生态系统生产力和ET验证期的R2分别为0.89和0.78。可见模型模拟结果的两个评价指标都处于较为理想的区间内, 说明WaSSI-C模型在研究区内具有较好的适用性。并对模型的蒸散计算方法进行了讨论, 在此基础上提出了模型中存在的问题和改进的方向。
刘宁,孙鹏森,刘世荣,孙阁. 流域水碳过程耦合模拟——WaSSI-C模型的率定与检验. 植物生态学报, 2013, 37(6): 492-502. DOI: 10.3724/SP.J.1258.2013.00051
LIU Ning,SUN Peng-Sen,LIU Shi-Rong,SUN Ge. Coupling simulation of water-carbon processes for catchment―calibration and validation of the WaSSI-C model. Chinese Journal of Plant Ecology, 2013, 37(6): 492-502. DOI: 10.3724/SP.J.1258.2013.00051
数据集 Dataset | 来源 Source | 用途 Usage | 分辨率 Resolution | 年 Year | |
---|---|---|---|---|---|
气象数据(气温和降水量) Climate data (air temperature and precipitation) | 国家气象局 State Meteorological Administration, China | 输入数据 Input data | 1 km × 1 km | 1988-2006 | |
植被覆盖数据 Vegetation cover data | 中分辨率成像光谱仪 Moderate Resolution Imaging Spectroradiometer (MODIS) ( | 输入数据 Input data | 1 km × 1 km | 2000 | |
叶面积指数 Leaf area index (LAI) | 中分辨率成像光谱仪 Moderate Resolution Imaging Spectroradiometer (MODIS) ( | 输入数据 Input data | 1 km × 1 km | 2000-2006 | |
土壤属性数据 Soil property data | 中国科学院南京土壤研究所 Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China | 输入数据 Input data | 1 km × 1 km | ||
总初级生产力 Gross primary production (GPP) | 中分辨率成像光谱仪 Moderate Resolution Imaging Spectroradiometer (MODIS) ( | 模型验证 Model validation | 1 km × 1 km | 2000-2006 | |
蒸散 Evapotranspiration (ET) | MODIS蒸散 MODIS_ET | 中分辨率成像光谱仪 Moderate Resolution Imaging Spectroradiometer (MODIS) ( | 模型验证 Model validation | 1 km × 1 km | 2000-2006 |
Zhang蒸散Zhang_ET | ET全球数据集 Global ET database ( | 模型验证 Model validation | 8 km × 8 km | 1988-2006 | |
径流数据 Runoff data (RUNOFF) | 四川省水文资源勘测局 Hydrology and Water Resource Investigation Bureau of Sichuan Province, China | 模型验证 Model validation | 1988-2006 |
表1 本研究中用到的数据集
Table 1 Datasets used in the study
数据集 Dataset | 来源 Source | 用途 Usage | 分辨率 Resolution | 年 Year | |
---|---|---|---|---|---|
气象数据(气温和降水量) Climate data (air temperature and precipitation) | 国家气象局 State Meteorological Administration, China | 输入数据 Input data | 1 km × 1 km | 1988-2006 | |
植被覆盖数据 Vegetation cover data | 中分辨率成像光谱仪 Moderate Resolution Imaging Spectroradiometer (MODIS) ( | 输入数据 Input data | 1 km × 1 km | 2000 | |
叶面积指数 Leaf area index (LAI) | 中分辨率成像光谱仪 Moderate Resolution Imaging Spectroradiometer (MODIS) ( | 输入数据 Input data | 1 km × 1 km | 2000-2006 | |
土壤属性数据 Soil property data | 中国科学院南京土壤研究所 Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China | 输入数据 Input data | 1 km × 1 km | ||
总初级生产力 Gross primary production (GPP) | 中分辨率成像光谱仪 Moderate Resolution Imaging Spectroradiometer (MODIS) ( | 模型验证 Model validation | 1 km × 1 km | 2000-2006 | |
蒸散 Evapotranspiration (ET) | MODIS蒸散 MODIS_ET | 中分辨率成像光谱仪 Moderate Resolution Imaging Spectroradiometer (MODIS) ( | 模型验证 Model validation | 1 km × 1 km | 2000-2006 |
Zhang蒸散Zhang_ET | ET全球数据集 Global ET database ( | 模型验证 Model validation | 8 km × 8 km | 1988-2006 | |
径流数据 Runoff data (RUNOFF) | 四川省水文资源勘测局 Hydrology and Water Resource Investigation Bureau of Sichuan Province, China | 模型验证 Model validation | 1988-2006 |
植被类型 Vegetation type | GEP = k × ET | REC = m + n × GEP | |||
---|---|---|---|---|---|
k ± SD | R2 | m ± SD | n ± SD | R2 | |
农田 Cropland | 3.13 ± 1.69 | 0.78 | 40.6 ± 3.84 | 0.43 ± 0.02 | 0.77 |
郁闭灌丛 Closed shrubland | 1.37 ± 0.62 | 0.77 | 11.4 ± 15.62 | 0.69 ± 0.15 | 0.74 |
落叶阔叶林 Deciduous broad-leaved forest | 3.20 ± 1.26 | 0.93 | 30.8 ± 2.93 | 0.45 ± 0.03 | 0.83 |
常绿阔叶林 Evergreen broad-leaved forest | 2.59 ± 0.54 | 0.92 | 19.6 ± 8.74 | 0.61 ± 0.06 | 0.63 |
常绿针叶林 Evergreen coniferous forest | 2.46 ± 0.96 | 0.89 | 9.9 ± 2.24 | 0.68 ± 0.03 | 0.80 |
草地 Grassland | 2.12 ± 1.66 | 0.84 | 18.9 ± 2.31 | 0.64 ± 0.02 | 0.82 |
混交林 Mixed forest | 2.74 ± 1.05 | 0.89 | 24.4 ± 4.24 | 0.62 ± 0.05 | 0.88 |
稀疏灌丛 Open shrubland | 1.33 ± 0.47 | 0.85 | 9.7 ± 3.03 | 0.56 ± 0.08 | 0.81 |
高山草甸 Alpine meadow | 1.26 ± 0.77 | 0.80 | 25.2 ± 3.23 | 0.53 ± 0.07 | 0.65 |
湿地 Wetland | 1.66 ± 1.33 | 0.78 | 7.8 ± 3.04 | 0.56 ± 0.03 | 0.80 |
表2 WaSSI-C模型主要植被类型的碳通量回归模型参数
Table 2 Parameters of main vegetation types for carbon flux regression model in WaSSI-C model
植被类型 Vegetation type | GEP = k × ET | REC = m + n × GEP | |||
---|---|---|---|---|---|
k ± SD | R2 | m ± SD | n ± SD | R2 | |
农田 Cropland | 3.13 ± 1.69 | 0.78 | 40.6 ± 3.84 | 0.43 ± 0.02 | 0.77 |
郁闭灌丛 Closed shrubland | 1.37 ± 0.62 | 0.77 | 11.4 ± 15.62 | 0.69 ± 0.15 | 0.74 |
落叶阔叶林 Deciduous broad-leaved forest | 3.20 ± 1.26 | 0.93 | 30.8 ± 2.93 | 0.45 ± 0.03 | 0.83 |
常绿阔叶林 Evergreen broad-leaved forest | 2.59 ± 0.54 | 0.92 | 19.6 ± 8.74 | 0.61 ± 0.06 | 0.63 |
常绿针叶林 Evergreen coniferous forest | 2.46 ± 0.96 | 0.89 | 9.9 ± 2.24 | 0.68 ± 0.03 | 0.80 |
草地 Grassland | 2.12 ± 1.66 | 0.84 | 18.9 ± 2.31 | 0.64 ± 0.02 | 0.82 |
混交林 Mixed forest | 2.74 ± 1.05 | 0.89 | 24.4 ± 4.24 | 0.62 ± 0.05 | 0.88 |
稀疏灌丛 Open shrubland | 1.33 ± 0.47 | 0.85 | 9.7 ± 3.03 | 0.56 ± 0.08 | 0.81 |
高山草甸 Alpine meadow | 1.26 ± 0.77 | 0.80 | 25.2 ± 3.23 | 0.53 ± 0.07 | 0.65 |
湿地 Wetland | 1.66 ± 1.33 | 0.78 | 7.8 ± 3.04 | 0.56 ± 0.03 | 0.80 |
评价指标 Evaluation index | 率定期 Calibration period (1988-1996) | 验证期 Validation period (1997-2006) |
---|---|---|
决定系数 Determined coefficient R2 | 0.86 | 0.78 |
Nash-Sutcliffe效率系数 Nash-Sutcliffe efficiency coefficient NS | 0.82 | 0.67 |
表3 率定期(1988-1996)和验证期(1997-2006)径流的评价指标值
Table 3 Evaluation index values of runoff during calibration period (1988-1996) and validation period (1997- 2006)
评价指标 Evaluation index | 率定期 Calibration period (1988-1996) | 验证期 Validation period (1997-2006) |
---|---|---|
决定系数 Determined coefficient R2 | 0.86 | 0.78 |
Nash-Sutcliffe效率系数 Nash-Sutcliffe efficiency coefficient NS | 0.82 | 0.67 |
图4 率定期(A)和验证期(B)流域月总径流(RUNOFF, mm·month-1)的WaSSI-C模拟值(点线)与观测值(实线)的对比。
Fig. 4 Comparison between total monthly runoff (RUNOFF, mm·month-1) simulated by WaSSI-C (dotted line) and observed (active line) in calibration period (A) and validation period (B).
图5 各水文响应单元(左)和流域总(右)平均月蒸散(ET, mm·month-1)的WaSSI-C模拟值与MODIS模拟值的对比。
Fig. 5 Comparison between mean monthly evapotranspiration (ET, mm·month-1) simulated by WaSSI-C and MODIS of each hydrology response unit (left) and the whole watershed (right).
图6 各水文响应单元(左)和流域总(右)平均月蒸散(ET, mm·month-1)的WaSSI-C模拟值与Zhang模拟值的对比。
Fig. 6 Comparison between mean monthly evapotranspiration (ET, mm·month-1) simulated by WaSSI-C and Zhang for each hydrology response unit (left) and the whole watershed (right).
图7 2000-2006年WaSSI-C、MODIS和Zhang模拟的平均月蒸散(ET, mm·month-1)的对比。
Fig. 7 Comparison of mean monthly evapotranspiration (ET, mm·month-1) simulated by WaSSI-C, MODIS and Zhang during the period of 2000-2006.
图8 各水文响应单元(左)和流域总(右)平均月总生态系统生产力(GEP, g C·m-2·month-1)的WaSSI-C模拟值与MODIS模拟值的对比。
Fig. 8 Comparison between mean monthly gross ecosystem productive (GEP) (g C·m-2·month-1) simulated by WaSSI-C and MODIS for each hydrology response unit (left) and the whole watershed (right).
图9 2000-2006年WaSSI-C、MODIS和Zhang模拟的平均月总生态系统生产力(GEP, g C·m-2·month-1)的对比。
Fig. 9 Comparison of mean monthly gross ecosystem productive (GEP) (g C·m-2·month-1) simulated by WaSSI-C, MODIS and Zhang during the period of 2000-2006.
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[1] | 刘宁, 孙鹏森, 刘世荣, 孙阁. WASSI-C生态水文模型响应单元空间尺度的确定——以杂古脑流域为例[J]. 植物生态学报, 2013, 37(2): 132-141. |
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