Figure 1: monthly precipitation and air temperature in 2006 and 2007 and their departures from the means of the previous 50 years (1956–2005) at the study.

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Figure 1: monthly precipitation and air temperature in 2006 and 2007 and their departures from the means of the previous 50 years (1956–2005) at the study site of East Ujimuqin of Inner Mongolia, China. From: Application of two remote sensing GPP algorithms at a semiarid grassland site of North China J Plant Ecol. 2011;4(4):302-312. doi:10.1093/jpe/rtr019 J Plant Ecol | © The Author 2011. Published by Oxford University Press on behalf of the Institute of Botany, Chinese Academy of Sciences and the Botanical Society of China. All rights reserved. For permissions, please email: journals.permissions@oup.com

Figure 6: linear relationships of EC GPP with (a) the temperature multiplier in the remote sensing GPP algorithms (i.e. T<sub>scalar</sub> in the VPM and T′ in the MODIS GPP algorithm) and (b) the moisture multiplier in the remote sensing GPP algorithms (i.e. W<sub>scalar</sub> in the VPM and VPD′ in the MODIS GPP algorithm) at the study site in East Ujimuqin of Inner Mongolia, China. From: Application of two remote sensing GPP algorithms at a semiarid grassland site of North China J Plant Ecol. 2011;4(4):302-312. doi:10.1093/jpe/rtr019 J Plant Ecol | © The Author 2011. Published by Oxford University Press on behalf of the Institute of Botany, Chinese Academy of Sciences and the Botanical Society of China. All rights reserved. For permissions, please email: journals.permissions@oup.com

Figure 7: linear relationship between VWC to a depth of 10 cm (m<sup>3</sup> m<sup>−3</sup>) and the moisture multiplier in the remote sensing algorithms (i.e. T<sub>scalar</sub> in the VPM and T′ in the MODIS GPP algorithm) at the study site in East Ujimuqin of Inner Mongolia, China. From: Application of two remote sensing GPP algorithms at a semiarid grassland site of North China J Plant Ecol. 2011;4(4):302-312. doi:10.1093/jpe/rtr019 J Plant Ecol | © The Author 2011. Published by Oxford University Press on behalf of the Institute of Botany, Chinese Academy of Sciences and the Botanical Society of China. All rights reserved. For permissions, please email: journals.permissions@oup.com

Figure 2: comparisons of the 8-day GPP measured by EC technique (EC GPP) with (a) the VPM predictions of GPP based on FPAR_EVI (GPP_VPM_EVI), (b) the VPM predictions of GPP based on FPAR_NDVI (GPP_VPM_NDVI), (c) the VPM predictions of GPP based on FPAR_MOD15 (GPP_VPM_MOD15), (d) the MODIS predictions of GPP based on FPAR_EVI (GPP_MOD_EVI), (e) the MODIS predictions of GPP based on FPAR_NDVI (GPP_MOD_NDVI), (f) the MODIS predictions of GPP based on FPAR_MOD15 (GPP_MOD_MOD15) and (g) the standard MODIS product (MOD17A2, C5) extracted by the geographical location of the study site, in East Ujimuqin of Inner Mongolia, China. In each graph, the dash or solid line is the best linear fit and doted line is the 1:1 reference. From: Application of two remote sensing GPP algorithms at a semiarid grassland site of North China J Plant Ecol. 2011;4(4):302-312. doi:10.1093/jpe/rtr019 J Plant Ecol | © The Author 2011. Published by Oxford University Press on behalf of the Institute of Botany, Chinese Academy of Sciences and the Botanical Society of China. All rights reserved. For permissions, please email: journals.permissions@oup.com

Figure 3: comparison of 8-day EC-measured GPP (EC GPP) with (a) the VPM predictions of GPP using various FPAR source, (b) the MODIS predictions of GPP using various FPAR source and (c) various FPAR estimates. From: Application of two remote sensing GPP algorithms at a semiarid grassland site of North China J Plant Ecol. 2011;4(4):302-312. doi:10.1093/jpe/rtr019 J Plant Ecol | © The Author 2011. Published by Oxford University Press on behalf of the Institute of Botany, Chinese Academy of Sciences and the Botanical Society of China. All rights reserved. For permissions, please email: journals.permissions@oup.com

Figure 4: scatter plots (a) (△, pre; •, mid and ▽, late indicate previous, middle and late stage of growing season, respectively) and path diagrams (b) illustrating the effects of four major environmental variables, i.e. air temperature at a height of 2 m (T<sub>a</sub>), PAR, VWC to a depth of 10 cm and VPD, on ecosystem GPP at a 8 day (b) time step at the study site of East Ujimuqin of Inner Mongolia, China. Lines with arrowhead indicate significant effects, and the values are the corresponding path coefficients. Solid lines indicate a positive effect and dashed lines a negative effect. From: Application of two remote sensing GPP algorithms at a semiarid grassland site of North China J Plant Ecol. 2011;4(4):302-312. doi:10.1093/jpe/rtr019 J Plant Ecol | © The Author 2011. Published by Oxford University Press on behalf of the Institute of Botany, Chinese Academy of Sciences and the Botanical Society of China. All rights reserved. For permissions, please email: journals.permissions@oup.com

Figure 5: linear relationships of EC GPP with three types of FPAR estimates (i.e. FPAR_EVI, FPAR_MOD15 and FPAR_NDVI) at the study site in East Ujimuqin of Inner Mongolia, China. From: Application of two remote sensing GPP algorithms at a semiarid grassland site of North China J Plant Ecol. 2011;4(4):302-312. doi:10.1093/jpe/rtr019 J Plant Ecol | © The Author 2011. Published by Oxford University Press on behalf of the Institute of Botany, Chinese Academy of Sciences and the Botanical Society of China. All rights reserved. For permissions, please email: journals.permissions@oup.com