当前位置： SCI文献检索 > GLOBAL CHANGE BIOLOGY期刊下所有文献 > Precipitation-drainage cycles lead to hot moments in soil carbon dioxide dynamics in a Neotropical wet forest.

Precipitation-drainage cycles lead to hot moments in soil carbon dioxide dynamics in a Neotropical wet forest.

Abstract：

:Soil CO2 concentrations and emissions from tropical forests are modulated seasonally by precipitation. However, subseasonal responses to meteorological events (e.g., storms, drought) are less well known. Here, we present the effects of meteorological variability on short-term (hours to months) dynamics of soil CO2 concentrations and emissions in a Neotropical wet forest. We continuously monitored soil temperature, moisture, and CO2 for a three-year period (2015-2017), encompassing normal conditions, floods, a dry El Niño period, and a hurricane. We used a coupled model (Hydrus-1D) for soil water propagation, heat transfer, and diffusive gas transport to explain observed soil moisture, soil temperature, and soil CO2 concentration responses to meteorology, and we estimated soil CO2 efflux with a gradient-flux model. Then, we predicted changes in soil CO2 concentrations and emissions under different warming climate change scenarios. Observed short-term (hourly to daily) soil CO2 concentration responded more to precipitation than to other meteorological variables (including lower pressure during the hurricane). Observed soil CO2 failed to exhibit diel patterns (associated with diel temperature fluctuations in drier climates), except during the drier El Niño period. Climate change scenarios showed enhanced soil CO2 due to warmer conditions, while precipitation played a critical role in moderating the balance between concentrations and emissions. The scenario with increased precipitation (based on a regional model projection) led to increases of +11% in soil CO2 concentrations and +4% in soil CO2 emissions. The scenario with decreased precipitation (based on global circulation model projections) resulted in increases of +4% in soil CO2 concentrations and +18% in soil CO2 emissions, and presented more prominent hot moments in soil CO2 outgassing. These findings suggest that soil CO2 will increase under warmer climate in tropical wet forests, and precipitation patterns will define the intensity of CO2 outgassing hot moments.

journal_name

Glob Chang Biol

journal_title

Global change biology

authors

Fernandez-Bou AS,Dierick D,Allen MF,Harmon TC

doi

10.1111/gcb.15194

subject

Has Abstract

pub_date

2020-09-01 00:00:00

pages

5303-5319

issue

eissn

1354-1013

issn

1365-2486

journal_volume

pub_type

杂志文章

在线工具

Precipitation-drainage cycles lead to hot moments in soil carbon dioxide dynamics in a Neotropical wet forest.