Global methane and nitrous oxide emissions from inland waters and estuaries
Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid
StandardStandard
Yn: Global Change Biology, Cyfrol 28, Rhif 15, 08.2022, t. 4713-4725.
Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid
HarvardHarvard
APA
CBE
MLA
VancouverVancouver
Author
RIS
TY - JOUR
T1 - Global methane and nitrous oxide emissions from inland waters and estuaries
AU - Zheng, Yajing
AU - Wu, Shuang
AU - Xiao, Shuqi
AU - Yu, Kai
AU - Fang, Xianto
AU - Xia, Longlong
AU - Wang, Jinyang
AU - Liu, Shuwei
AU - Freeman, Chris
AU - Zou, Jianwen
PY - 2022/8
Y1 - 2022/8
N2 - AbstractInland waters (rivers, reservoirs, lakes, ponds, streams) and estuaries are significant emitters of methane (CH4) and nitrous oxide (N2O) to the atmosphere, while global estimates of these emissions have been hampered due to the lack of a worldwide comprehensive data set of CH4 and N2O flux components. Here, we synthesize 2997 in‐situ flux or concentration measurements of CH4 and N2O from 277 peer‐reviewed publications to estimate global CH4 and N2O emissions from inland waters and estuaries. Inland waters including rivers, reservoirs, lakes, and streams together release 95.18 Tg CH4 year−1 (ebullition plus diffusion) and 1.48 Tg N2O year−1 (diffusion) to the atmosphere, yielding an overall CO2‐equivalent emission total of 3.06 Pg CO2 year−1. The estimate of CH4 and N2O emissions represents roughly 60% of CO2 emissions (5.13 Pg CO2 year−1) from these four inland aquatic systems, among which lakes act as the largest emitter for both CH4 and N2O. Ebullition showed as a dominant flux component of CH4, contributing up to 62%–84% of total CH4 fluxes across all inland waters. Chamber‐derived CH4 emission rates are significantly greater than those determined by diffusion model‐based methods for commonly capturing of both diffusive and ebullitive fluxes. Water dissolved oxygen (DO) showed as a dominant factor among all variables to influence both CH4 (diffusive and ebullitive) and N2O fluxes from inland waters. Our study reveals a major oversight in regional and global CH4 budgets from inland waters, caused by neglecting the dominant role of ebullition pathways in those emissions. The estimated indirect N2O EF5 values suggest that a downward refinement is required in current IPCC default EF5 values for inland waters and estuaries. Our findings further indicate that a comprehensive understanding of the magnitude and patterns of CH4 and N2O emissions from inland waters and estuaries is essential in defining the way of how these aquatic systems will shape our climate.
AB - AbstractInland waters (rivers, reservoirs, lakes, ponds, streams) and estuaries are significant emitters of methane (CH4) and nitrous oxide (N2O) to the atmosphere, while global estimates of these emissions have been hampered due to the lack of a worldwide comprehensive data set of CH4 and N2O flux components. Here, we synthesize 2997 in‐situ flux or concentration measurements of CH4 and N2O from 277 peer‐reviewed publications to estimate global CH4 and N2O emissions from inland waters and estuaries. Inland waters including rivers, reservoirs, lakes, and streams together release 95.18 Tg CH4 year−1 (ebullition plus diffusion) and 1.48 Tg N2O year−1 (diffusion) to the atmosphere, yielding an overall CO2‐equivalent emission total of 3.06 Pg CO2 year−1. The estimate of CH4 and N2O emissions represents roughly 60% of CO2 emissions (5.13 Pg CO2 year−1) from these four inland aquatic systems, among which lakes act as the largest emitter for both CH4 and N2O. Ebullition showed as a dominant flux component of CH4, contributing up to 62%–84% of total CH4 fluxes across all inland waters. Chamber‐derived CH4 emission rates are significantly greater than those determined by diffusion model‐based methods for commonly capturing of both diffusive and ebullitive fluxes. Water dissolved oxygen (DO) showed as a dominant factor among all variables to influence both CH4 (diffusive and ebullitive) and N2O fluxes from inland waters. Our study reveals a major oversight in regional and global CH4 budgets from inland waters, caused by neglecting the dominant role of ebullition pathways in those emissions. The estimated indirect N2O EF5 values suggest that a downward refinement is required in current IPCC default EF5 values for inland waters and estuaries. Our findings further indicate that a comprehensive understanding of the magnitude and patterns of CH4 and N2O emissions from inland waters and estuaries is essential in defining the way of how these aquatic systems will shape our climate.
KW - estimate
KW - estuaries
KW - indirect emission factor
KW - inland waters
KW - methane
KW - nitrous oxide
KW - General Environmental Science
KW - Ecology
KW - Global and Planetary Change
KW - Environmental Chemistry
U2 - 10.1111/gcb.16233
DO - 10.1111/gcb.16233
M3 - Article
VL - 28
SP - 4713
EP - 4725
JO - Global Change Biology
JF - Global Change Biology
SN - 1365-2486
IS - 15
ER -