Preprints
https://doi.org/10.5194/bg-2021-57
https://doi.org/10.5194/bg-2021-57

  19 Mar 2021

19 Mar 2021

Review status: a revised version of this preprint was accepted for the journal BG and is expected to appear here in due course.

Quantifying the role of moss in terrestrial ecosystem carbon dynamics in northern high-latitudes

Junrong Zha and Qianlai Zhuang Junrong Zha and Qianlai Zhuang
  • Department of Earth, Atmospheric, and Planetary Sciences and Department of Agronomy, Purdue University, West Lafayette, IN 47907, USA

Abstract. In addition to woody and herbaceous plants, mosses are ubiquitous in northern terrestrial ecosystems, which play an important role in regional carbon, water and energy cycling. Current global land surface models without considering moss may bias the quantification of the regional carbon dynamics. Here we incorporate moss into a process-based biogeochemistry model, the Terrestrial Ecosystem Model (TEM 5.0), as a new plant functional type to develop a new model (TEM_Moss). The new model explicitly quantifies the interactions between higher plants and mosses and their competition for energy, water, and nutrient. Compared to the estimates using TEM 5.0, the new model estimates that the regional terrestrial soils store 132.7 Pg more C at present day, and will store 157.5 Pg and 179.1 Pg more C under the RCP 8.5 and RCP 2.6 scenarios, respectively, by the end of the 21st century. Ensemble regional simulations forced with different parameters for the 21st century with TEM_Moss predict that the region will accumulate 161.1 ± 142.1 Pg C under the RCP 2.6 scenario, and 186.7 ± 166.1 Pg C under the RCP 8.5 scenario over the century. Our study highlights the necessity of coupling moss into Earth System Models to adequately quantify terrestrial carbon-climate feedbacks in the Arctic.

Junrong Zha and Qianlai Zhuang

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on bg-2021-57', Anonymous Referee #1, 26 Mar 2021
    • AC1: 'Reply on RC1', Junrong Zha, 02 Jun 2021
    • AC3: 'Reply on RC1', Junrong Zha, 02 Jun 2021
    • AC4: 'Reply on RC1', Junrong Zha, 02 Jun 2021
  • RC2: 'Comment on bg-2021-57', Anonymous Referee #2, 27 Apr 2021
    • AC2: 'Reply on RC2', Junrong Zha, 02 Jun 2021
    • AC5: 'Reply on RC2', Junrong Zha, 02 Jun 2021

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on bg-2021-57', Anonymous Referee #1, 26 Mar 2021
    • AC1: 'Reply on RC1', Junrong Zha, 02 Jun 2021
    • AC3: 'Reply on RC1', Junrong Zha, 02 Jun 2021
    • AC4: 'Reply on RC1', Junrong Zha, 02 Jun 2021
  • RC2: 'Comment on bg-2021-57', Anonymous Referee #2, 27 Apr 2021
    • AC2: 'Reply on RC2', Junrong Zha, 02 Jun 2021
    • AC5: 'Reply on RC2', Junrong Zha, 02 Jun 2021

Junrong Zha and Qianlai Zhuang

Junrong Zha and Qianlai Zhuang

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Short summary
This study incorporated moss into an extant biogeochemistry model to simulate the role of moss in carbon dynamics in the Arctic. The interactions between higher plants and mosses and their competition for energy, water, and nutrient are considered in our study. We found that, compared with the previous model without moss, the new model estimated a much higher carbon accumulation in the region during last and this century.
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