The steady growth of CO 2 during the dry season (November to May) indicates a decreasing trend of vegetation uptake in the neighbouring regions (Fig. 4 a).
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Diurnal and seasonal variability of CO<sub>2</sub> and CH<sub>4</sub> concentration in a semi-urban environment of western India.
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The sentences
The water vapour variation in the upper troposphere and lower stratosphere is highly significant due to its impact on global warming.