Carbon dioxide (CO2) is the most important greenhouse gas influencing the Earth’s climate; therefore accurate modeling of its variability has paramount significance. In this regard, we have performed the simulation of CO2 residue (i.e., detrended deseasonalised CO2) based on input of meteorological parameters (temperature, humidity, pressure and wind), El Niño index, sea surface temperature, and Normalized Difference Vegetation Index in a machine learning (ML) model. Long-term observations available from the World Data Centre for Greenhouse Gases (WDCGG) and the National Oceanic and Atmospheric Administration (NOAA) have been used for training and validation of ML model. Model successfully reproduced 72% of observed variability in CO2 residue with an error of 0.45 ppmv over Mauna Loa (19.54° N; - 155.58° E). The cumulative temperature anomaly is found to play a key role in the simulation of CO2 residue over Mauna Loa. Evaluation reveals a reasonably good agreement between modelled and observed CO2 residue (R2=0.20–0.55 and RMSE=20–60%) over regional sites and for global mean CO2. However, the model shows limitation in capturing spikes likely caused by strong local influences. Inclusion of additional input parameters, representing local anthropogenic influences, is recommended to further improve the model performance over regional sites. Our study demonstrates the potential of ML modeling for the simulations of CO2 variability to complement the computationally expensive climate models.
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Applicability of machine learning model to simulate atmospheric CO2 variability
Semantic Scholar · Environmental Science · 2022
Abstract
Carbon dioxide (CO2) is the most important greenhouse gas influencing the Earth’s climate; therefore accurate modeling of its variability has paramount significance. In this regard, we have performed the simulation of CO2 residue (i.e., detrended deseasonalised CO2) based on input of meteorological parameters (temperature, humidity, pressure and wind), El Niño index, sea surface temperature, and Normalized Difference Vegetation Index in a machine learning (ML) model. Long-term observations available from the World Data Centre for Greenhouse Gases (WDCGG) and the National Oceanic and Atmospheric Administration (NOAA) have been used for training and validation of ML model. Model successfully reproduced 72% of observed variability in CO2 residue with an error of 0.45 ppmv over Mauna Loa (19.54° N; - 155.58° E). The cumulative temperature anomaly is found to play a key role in the simulation of CO2 residue over Mauna Loa. Evaluation reveals a reasonably good agreement between modelled and observed CO2 residue (R2=0.20–0.55 and RMSE=20–60%) over regional sites and for global mean CO2. However, the model shows limitation in capturing spikes likely caused by strong local influences. Inclusion of additional input parameters, representing local anthropogenic influences, is recommended to further improve the model performance over regional sites. Our study demonstrates the potential of ML modeling for the simulations of CO2 variability to complement the computationally expensive climate models.