Refined estimate of China's CO2 emissions in spatiotemporal distributions
Atmos. Chem. Phys., 13, 10873-10882, 2013
Observed small spatial scale and seasonal variability of the CO2 system in the Southern Ocean
Biogeosciences, 11, 75-90, 2014
Soil greenhouse gas fluxes from different tree species on Taihang Mountain, North China
Biogeosciences, 11, 1649-1666, 2014
Estimating Asian terrestrial carbon fluxes from CONTRAIL aircraft and surface CO2 observations for the period 2006–2010
Atmos. Chem. Phys., 14, 5807-5824, 2014
Quantifying the biophysical climate change mitigation potential of Canada's forest sector
Biogeosciences, 11, 3515-3529, 2014
Simulating the integrated summertime Δ14CO2 signature from anthropogenic emissions over Western Europe
Atmos. Chem. Phys., 14, 7273-7290, 2014
High-precision quasi-continuous atmospheric greenhouse gas measurements at Trainou tower (Orléans forest, France)
Atmos. Meas. Tech., 7, 2283-2296, 2014
Interannual sea–air CO2 flux variability from an observation-driven ocean mixed-layer scheme
Biogeosciences, 11, 4599-4613, 2014
Estimating the carbon dynamics of South Korean forests from 1954 to 2012
Biogeosciences, 11, 4637-4650, 2014
Greenhouse gas network design using backward Lagrangian particle dispersion modelling − Part 1: Methodology and Australian test case
Atmos. Chem. Phys., 14, 9363-9378, 2014
Biogeophysical feedbacks enhance the Arctic terrestrial carbon sink in regional Earth system dynamics
Biogeosciences, 11, 5503-5519, 2014
Constraint of soil moisture on CO2 efflux from tundra lichen, moss, and tussock in Council, Alaska, using a hierarchical Bayesian model
Biogeosciences, 11, 5567-5579, 2014
Winter-to-summer evolution of pCO2 in surface water and air–sea CO2 flux in the seasonal ice zone of the Southern Ocean
Biogeosciences, 11, 5749-5761, 2014
Explaining the seasonal cycle of the globally averaged CO2 with a carbon-cycle model
Earth Syst. Dynam., 5, 345-354, 2014
Biophsyical constraints on gross primary production by the terrestrial biosphere
Biogeosciences, 11, 5987-6001, 2014
Impacts of freezing and thawing dynamics on foliar litter carbon release in alpine/subalpine forests along an altitudinal gradient in the eastern Tibetan Plateau
Summary: A 2-year field litter decomposition experiment was conducted along an altitudinal gradient in the eastern Tibetan Plateau. More rapid 2-year C is released from fresh foliar litter at upper elevations compared to lower elevations. However, high C release was observed at low altitudes during winter, but high altitudes exhibited high C release during growing season. The results suggested that the onset of C release in fresh litter could delay in this cold region in the scenario of climate warming.
Biogeosciences, 11, 6471-6481, 2014
Continued increase in atmospheric CO2 seasonal amplitude in the 21st century projected by the CMIP5 Earth system models
Summary: This paper presents the CMIP5 model predictions on the seasonal characteristics of global carbon cycle. We show a model consensus that the amplitude of this seasonal cycle will increase in the future under the RCP8.5 emission scenario. This is mostly due to enhanced ecosystem productivity in high latitude regions. While the models' ensemble CO2 amplitude increase is close to observation, our results suggest the underlying mechanisms may not be realistic.
Earth Syst. Dynam., 5, 423-439, 2014
Effect of ablation rings and soil temperature on 3-year spring CO2 efflux along the Dalton Highway, Alaska
Biogeosciences, 11, 6539-6552, 2014
Terrestrial cycling of 13CO2 by photosynthesis, respiration, and biomass burning in SiBCASA
Biogeosciences, 11, 6553-6571, 2014
Using atmospheric observations to evaluate the spatiotemporal variability of CO2 fluxes simulated by terrestrial biospheric models
Summary: Terrestrial biospheric models (TBMs) are used to assess carbon--climate interactions. We present a new and complementary approach for evaluating the spatiotemporal patterns, rather than magnitudes, of biosphere--atmosphere carbon exchange predicted by TBMs, based on atmospheric observations. Experiments demonstrate that the performance of TBMs varies substantially across seasons and biomes, with best performance during the growing season and more limited skill during transition seasons.
Biogeosciences, 11, 6985-6997, 2014
A joint data assimilation system (Tan-Tracker) to simultaneously estimate surface CO2 fluxes and 3-D atmospheric CO2 concentrations from observations
Summary: A new carbon cycle data assimilation system (Tan-Tracker) is developed based on an advanced hybrid assimilation approach, as a part of the preparation for the launch of the Chinese carbon dioxide observation satellite (TanSat). Tan-Tracker adopts a joint data assimilation framework to simultaneously estimate CO2 concentrations and CFs and thus gradually reduce the uncertainty in the CO2 concentration evolution through continuously fitting model CO2 concentration simulations to the observations.
Atmos. Chem. Phys., 14, 13281-13293, 2014
Influence of CO2 observations on the optimized CO2 flux in an ensemble Kalman filter
Atmos. Chem. Phys., 14, 13515-13530, 2014
Comparison of continuous in situ CO2 observations at Jungfraujoch using two different measurement techniques
Atmos. Meas. Tech., 8, 57-68, 2015
Two perspectives on the coupled carbon, water and energy exchange in the planetary boundary layer
Summary: This study investigates the interactions among the carbon, water and heat cycles above a maize field at the diurnal scale. We couple two land-surface schemes, corresponding to two different modelling approaches, to the same atmospheric boundary-layer (ABL) model. We find the simpler meteorological approach best reproduces the surface and upper-air observations. Finally, we show that the interaction of subsidence with ABL dynamics is key to explain the daytime atmospheric CO2 budget.
Biogeosciences, 12, 103-123, 2015
Evaluating the ocean biogeochemical components of Earth system models using atmospheric potential oxygen and ocean color data
Summary: The observed seasonal cycles in atmospheric potential oxygen (APO) at five surface monitoring sites are compared to those inferred from the air-sea O2 fluxes of six ocean biogeochemistry models. The simulated air-sea fluxes are translated into APO seasonal cycles using a matrix method that takes into account atmospheric transport model (ATM) uncertainty among 13 different ATMs. Net primary production (NPP), estimated from satellite ocean color data, is also compared to model output.
Biogeosciences, 12, 193-208, 2015
Atmospheric inversion of surface carbon flux with consideration of the spatial distribution of US crop production and consumption
Summary: The major findings of this article are the following. 1. Atmospheric CO2 observations alone are not sufficient to estimate the spatial distribution of carbon sources and sinks over North America, even though it is one of the most densely observed regions in the world. 2. To improve atmospheric inversion, lateral carbon transfer in agricultural products should be considered in the prior flux used to constrain the inversion.
Biogeosciences, 12, 323-343, 2015
Recent changes in the global and regional carbon cycle: analysis of first-order diagnostics
Summary: Recent papers suggest a slow-down in the natural uptake of anthropogenic CO2. We analyse recent trends in atmospheric concentration and known inputs to test for such a slow-down. We see, rather, an increase in uptake compared to a simple response to changing CO2 concentration. Using atmospheric models and statistical techniques we isolate this increased uptake to the northern temperate and boreal continents during summer, suggesting a stronger growing season.
Biogeosciences, 12, 835-844, 2015
Effects of land management on large trees and carbon stocks
Biogeosciences, 12, 855-862, 2015
Uncertainty analysis of eddy covariance CO2 flux measurements for different EC tower distances using an extended two-tower approach
Summary: This study introduces an extension of the classical two-tower approach for uncertainty estimation of measured net CO2 fluxes (NEE). Because land surface properties cannot be assumed identical at two eddy covariance towers, a correction for systematic flux differences is proposed to be added to the classical weather filter. With this extension, the overestimation of NEE uncertainty due to systematic flux differences (which are assumed to increase with tower distance) can considerably be reduced.
Biogeosciences, 12, 1205-1221, 2015
Greenhouse gas network design using backward Lagrangian particle dispersion modelling – Part 2: Sensitivity analyses and South African test case
Summary: This study aims to provide an optimal network design for the placement of new atmospheric monitoring stations around South Africa, to best estimate the emission and uptake of carbon dioxide fluxes due to both anthropogenic and natural sources. In addition, a sensitivity analysis was performed on the impact that certain parameters would have on the final network solution, considering the inverse modelling framework, the transport model and the use of a different optimisation routine.
Atmos. Chem. Phys., 15, 2051-2069, 2015
Investigating bias in the application of curve fitting programs to atmospheric time series
Atmos. Meas. Tech., 8, 1469-1489, 2015