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Validation of collection of 6 MODIS/Terra and MODIS/Aqua gross primary production in an alpine meadow of the Northern Tibetan Plateau

机译:在青藏高原北部高寒草甸收集6种MODIS / Terra和MODIS / Aqua初级生产总值的验证

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摘要

Moderate Resolution Imaging Spectroradiometer (MODIS) continuously monitors gross primary production (GPP), which is an extremely important component of carbon cycling, at the global scale. Uncertainties about MODIS GPP limit our ability to accurately quantify GPP at the regional scales. The Collection 6 MODIS/Terra and MODIS/Aqua GPP products (i.e. MOD17A2H and MYD17A2H) were compared with the estimated GPP (GPPEC) by eddy covariance measurements in an alpine meadow in the Northern Tibetan Plateau during three consecutive growing seasons of 2005-2007. The Collection 6 MODIS/Terra and MODIS/Aqua fractional photosynthetically active radiation (FPAR) products (i.e. MOD15A2H and MYD15A2H) were also validated. The MOD17A2H and MYD17A2H products tended to overestimate GPPEC by 2.17% and 7.35% in 2005-2007, respectively, although these differences were not significant. The MOD15A2H and MYD15A2H products also tended to overestimate ground-based FPAR (FPAR(G)) by 20.31% and 24.73% in 2005-2007, respectively. The overestimation of FPAR resulted in about 17.51-23.97% overestimation of GPPEC. The default maximum light-use efficiency (emax) of 0.86 g C MJ(-1) only underestimated the ground-based emax (0.88 g C MJ(-1)) by 2.27%, which in turn resulted in about 2.13-2.72% underestimation of GPPEC. The meteorology data errors only caused about 0.48-1.06% underestimation of GPPEC. Therefore, although MODIS Collection 6 GPP had a very high accuracy, the input parameters had relative greater errors in the alpine meadow of the Northern Tibetan Plateau. The differences between MODIS GPP and GPPEC mainly resulted from FPAR, followed by emax and meteorological data.
机译:中分辨率成像光谱仪(MODIS)在全球范围内连续监测初级生产总值(GPP),这是碳循环的极其重要的组成部分。关于MODIS GPP的不确定性限制了我们在区域范围内准确量化GPP的能力。在2005-2007年的三个连续生长季节中,通过涡度协方差测量将藏6 MODIS / Terra和MODIS / Aqua GPP产品(即MOD17A2H和MYD17A2H)与估计的GPP(GPPEC)进行了比较。还对Collection 6 MODIS / Terra和MODIS / Aqua分数光合有效辐射(FPAR)产品(即MOD15A2H和MYD15A2H)进行了验证。 MOD17A2H和MYD17A2H产品在2005-2007年期间倾向于分别高估GPPEC 2.17%和7.35%,尽管这些差异并不明显。 2005-2007年,MOD15A2H和MYD15A2H产品也往往分别高估了地面FPAR(FPAR(G))20.31%和24.73%。 FPAR的高估导致GPPEC的高估约17.51-23.97%。默认的最大光使用效率(emax)为0.86 g C MJ(-1)仅低估了地面emax(0.88 g C MJ(-1))2.27%,这反过来导致大约2.13-2.72%低估了GPPEC。气象数据错误仅引起GPPEC低估约0.48-1.06%。因此,尽管MODIS Collection 6 GPP具有非常高的精度,但输入参数在青藏高原北部的高山草甸中具有相对较大的误差。 MODIS GPP和GPPEC之间的差异主要是由FPAR引起的,其次是emax和气象数据。

著录项

  • 来源
    《International journal of remote sensing》 |2017年第16期|4517-4534|共18页
  • 作者单位

    Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Lhasa Plateau Ecosyst Res Stn, Beijing, Peoples R China;

    Beijing Normal Univ, Sch Geog, Beijing, Peoples R China;

    Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Lhasa Plateau Ecosyst Res Stn, Beijing, Peoples R China;

    Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Lhasa Plateau Ecosyst Res Stn, Beijing, Peoples R China|Univ Chinese Acad Sci, Coll Resources & Environm, Beijing, Peoples R China;

    Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Lhasa Plateau Ecosyst Res Stn, Beijing, Peoples R China|Univ Chinese Acad Sci, Coll Resources & Environm, Beijing, Peoples R China;

    Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Lhasa Plateau Ecosyst Res Stn, Beijing, Peoples R China|Univ Chinese Acad Sci, Coll Resources & Environm, Beijing, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
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