Dennis D. Baldocchi, Kadmiel Maseyk, Yuji Kominami, Nadine K. Ruehr, Patrick M. Crill, John E. Drake, Mioko Ataka, Anya M. Hopple, Haiming Kan, Samaneh Ashraf, Matthew Saunders, Zhuo Pang, Daphne Szutu, Stephanie C. Pennington, Whendee L. Silver, Scott T. Miller, Cecilio Oyonarte, David A. Lipson, Naishen Liang, Masahito Ueyama, Thomas Wutzler, Michael L. Goulden, Järvi Järveoja, Jiye Zeng, Wu Sun, Debjani Sihi, Takashi Hirano, Nina Buchmann, Amir AghaKouchak, Peter S. Curtis, Ruth K. Varner, Greg Winston, Munemasa Teramoto, Mark G. Tjoelker, Susan E. Trumbore, Kathleen Savage, Omar Gutiérrez del Arroyo, Asko Noormets, Mats Nilsson, Catriona A. Macdonald, Carolyn Monika Görres, M. Altaf Arain, Alexandre A. Renchon, Joseph Verfaillie, James W. Raich, Masahiro Takagi, Jason P. Kaye, Quan Zhang, Hamidreza Norouzi, Ulli Seibt, Melanie A. Mayes, Jinsong Wang, Juan J. Armesto, Marion Schrumpf, Tianshan Zha, Mirco Migliavacca, Chelcy Ford Miniat, Jin-Sheng He, Enrique P. Sánchez-Cañete, Michael Gavazzi, Tarek S. El-Madany, T. A. Black, H. Hughes, Elise Pendall, Christopher M. Gough, Jillian W. Gregg, Guofang Miao, Junliang Zou, Avni Malhotra, Russell L. Scott, D. S. Christianson, Marguerite Mauritz, Steve McNulty, Juying Wu, Jinshi Jian, K. C. Mathes, Tana E. Wood, Rodrigo Vargas, Jennifer Goedhart Nietz, Christoph S. Vogel, Claire L. Phillips, Mariah S. Carbone, Kentaro Takagi, Shih-Chieh Chang, Jorge F. Perez-Quezada, Richard P. Phillips, Hassan Anjileli, Eric A. Davidson, Ankur R. Desai, Christine S. O’Connell, Matthias Peichl, Bruce Osborne, Ben Bond-Lamberty, and Rachhpal S. Jassal
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and it is critical to understand how soil greenhouse gas (GHG) emissions and uptake will respond to ongoing climate change. In particular, the soil‐to‐atmosphere CO2 flux, commonly though imprecisely termed soil respiration (R S), is one of the largest carbon fluxes in the Earth system. An increasing number of high‐frequency R S measurements (typically, from an automated system with hourly sampling) have been made over the last two decades; an increasing number of methane measurements are being made with such systems as well. Such high frequency data are an invaluable resource for understanding GHG fluxes, but lack a central database or repository. Here we describe the lightweight, open‐source COSORE (COntinuous SOil REspiration) database and software, that focuses on automated, continuous and long‐term GHG flux datasets, and is intended to serve as a community resource for earth sciences, climate change syntheses and model evaluation. Contributed datasets are mapped to a single, consistent standard, with metadata on contributors, geographic location, measurement conditions and ancillary data. The design emphasizes the importance of reproducibility, scientific transparency and open access to data. While being oriented towards continuously measured R S, the database design accommodates other soil‐atmosphere measurements (e.g. ecosystem respiration, chamber‐measured net ecosystem exchange, methane fluxes) as well as experimental treatments (heterotrophic only, etc.). We give brief examples of the types of analyses possible using this new community resource and describe its accompanying R software package., Here we describe the lightweight, open source COSORE (COntinuous SOil REspiration) database and software. COSORE focuses on automated, continuous and long‐term greenhouse gas flux datasets, and is intended to serve as a community resource for earth sciences, climate change syntheses and model evaluation.