Severe Long‐Lasting Drought Accelerated Carbon Depletion in the Mongolian Plateau. Issue 10 (25th May 2019)

• Record Type: Journal Article
• Authors: Lu, Chaoqun; Tian, Hanqin; Zhang, Jien; Yu, Zhen; Pan, Shufen; Dangal, Shree; Zhang, Bowen; Yang, Jia; Pederson, Neil; Hessl, Amy
• Is Part Of: Geophysical research letters. Volume 46:Issue 10(2019)
• Page Start: 5303
• Page End: 5312
• Publication Date: 2019-05-25
• Subjects: net ecosystem production -- long‐lasting drought -- arid and semiarid ecosystems -- carbon dynamics -- ecosystem modeling -- the Mongolian Plateau; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1029/2018GL081418
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: Paleoclimate records identified a severe drought lasting approximately a decade on the Mongolian Plateau during the 2000s, the severity of which was only exceeded by a single drought during the last two millennia. Under high‐emission scenarios, arid and semiarid areas are projected to continue to experience a drying trend over the coming decades; therefore, understanding how ecosystems respond to long‐lasting drought has global implications. Here we used a process‐based ecosystem model to examine the interannual and intra‐annual variations in net ecosystem productivity in response to climate extremes across the Mongolian Plateau. We find that the recent‐decade drought caused Mongolian terrestrial ecosystems to shift from a carbon (C) sink to a C source, canceling 40% of climate‐induced C accumulation over the entire twentieth century. Our study details a shortened C sequestering season, increased summer C source, and accelerated C depletion during the 2000s drought. Plain Language Summary: Multiple lines of evidence have shown detrimental effects of drought events on ecosystem production and carbon dynamics, but it remains uncertain how arid and semiarid ecosystems respond to long‐lasting drought. Here we reveal that a severe drought during the first decade of the 2000s on the Mongolian Plateau considerably weakened C sequestration capacity and accelerated C depletion. This work has broad implications for understanding impacts of persistent droughts on terrestrial C dynamics as a drying trend, in many arid and semiarid areas, is projected to continue over the coming decades. Key Points: The recent decade (2000–2009) has been identified as one of the driest periods on the Mongolian Plateau over the most recent ~2, 000 years This long‐duration drought shortened the C sequestration season, increased the summer C source, and led to a net annual C release The NEP amplitude in this dry decade increased due to reduced C uptake and increased C emissions, implying an accelerated C depletion