From 1992 to 2014, CCT increased at a rate of 0.48 TgC yr −1 , accounting for 2.59% of annual CCT. The given regional area (RA) varied little among years, and MCT dominated the pattern of CCT, exhibiting an increasing trend (Fig. 3b ) at a rate of 3.34 gC m −2 yr −1 .
← all excerpts
Divergent drivers of the spatial and temporal variations of cropland carbon transfer in Liaoning province, China.
2
—
—
The sentences
Results The spatial variations of CCT and its components From 1992–2014, the CCT of Liaoning province was 18.56 TgC yr −1 and spatially varied, exhibiting a decreasing trend from northwest to southeast (Fig. 2a ).