ABSTRACT
Lakes are ‘hotspots’ for greenhouse gas (GHG) emissions, primarily carbon dioxide (CO2) and methane (CH4). Understanding the processes regulating GHG emissions from lakes, and their temporal variability, is essential for more accurately quantifying the role of lakes in global GHG cycles. In this study, we identified the processes that affect CO2 and CH4 concentrations in a small (0.3 km2) eutrophic monomictic lake (Okaro, New Zealand). A mass balance model was used to calculate changes in CO2 and CH4 storage in the lake as a result of internal cycling and atmospheric fluxes. To support model computations, CO2 and CH4 concentrations profiles were measured monthly over a one-year period, in addition to temperature, dissolved oxygen and chlorophyll a. Annually, Lake Okaro acted as a sink of CO2 from the atmosphere (425.4 mmol CO2 m−2 y−1) and a source of CH4 (553.4 mmol CH4 m−2 y−1) equating to a net GHG emission (diffusive fluxes of CO2 and CH4 combined) of 0.22 kg CO2-eq m−2 y−1. Although it may be viewed as conservative and applies only to diffusive fluxes, our study indicates that eutrophic lakes with high rates of primary production may act as a net source of GHGs.
Acknowledgement
We thank the Bay of Plenty Regional Council (BOPRC) for technical support, and Paul Scholes of BOPRC for data provision. Special thanks to Joseph Butterworth (BOPRC) for field work assistance and Janine Ryburn (The University of Waikato) for helpful support in laboratory analysis. ABS: Conceptualisation, Methodology, Software, Validation, Formal Analysis, Investigation, Writing – Original Draft, Writing – Reviewing and Editing, DPH: Funding acquisition, Supervision, Resources, Writing – Reviewing and Editing. LAS: Supervision, Resources, Reviewing and Editing. ISO: Writing – Reviewing and Editing. CHH: Supervision.
Disclosure statement
No potential conflict of interest was reported by the author(s).