CO2 variability over a tropical coastal station in India: Synergy of observation and model

K N Uma; Imran A Girach; Naveen Chandra; Prabir K Patra; N V P Kiran Kumar; Prabha R Nair

doi:10.1016/j.scitotenv.2024.177371

CO₂ variability over a tropical coastal station in India: Synergy of observation and model

Sci Total Environ. 2024 Nov 19:957:177371. doi: 10.1016/j.scitotenv.2024.177371. Online ahead of print.

Authors

K N Uma¹, Imran A Girach², Naveen Chandra³, Prabir K Patra⁴, N V P Kiran Kumar⁵, Prabha R Nair⁶

Affiliations

¹ Space Physics Laboratory, Vikram Sarabhai Space Centre, Thiruvananthapuram 695022, India. Electronic address: uma_kn@vssc.gov.in.
² Space Applications Centre, Indian Space Research Organisation, Ahmedabad 380015, India. Electronic address: imran.girach@gmail.com.
³ Research Institute for Global Change, JAMSTEC, Yokohama 2360001, Japan.
⁴ Research Institute for Global Change, JAMSTEC, Yokohama 2360001, Japan; Research Institute for Humanity and Nature, Kyoto 6038047, Japan; Graduate School of Science, Tohoku University, Sendai 9808578, Japan.
⁵ Space Physics Laboratory, Vikram Sarabhai Space Centre, Thiruvananthapuram 695022, India.
⁶ TC 95/1185, Aiswarya Gardens, Kumarapuram, Thiruvananthapuram 695011, India; formerly at Space Physics Laboratory, Vikram Sarabhai Space Centre, Thiruvananthapuram 695022, India.

PMID: 39500448
DOI: 10.1016/j.scitotenv.2024.177371

Abstract

Carbon dioxide (CO₂), being the prime greenhouse gas, has largest contribution in radiative forcing and global warming due to increased anthropogenic emissions leading to regional and global climate change. We performed CO₂ measurements using a continuous monitoring instrument at a tropical coastal station at the southern tip of India (Thumba; 8.54° N, 76.86° E) during 2017-2021. Combining measurements with model simulations and satellite observations, present study aims to understand CO₂ variabilities, contribution of various sources and role of dynamics. The observed trend of 2.19 ppm y^-1 is well simulated (2.47 ppm y^-1) by the chemistry-transport model (MIROC4-ACTM), which is contributed by trends in fossil fuel (4.59 ppm y^-1), biosphere (-1.46 ppm y^-1) and ocean (-0.66 ppm y^-1) tracers of CO₂ flux. Mean seasonal cycle with amplitude of about 8 ppm is observed, with a maximum during premonsoon (April) and minimum at the end of the monsoon season (September). The model reproduced the observed seasonal cycle well (r² = 0.89) and showed that the seasonal peak is predominantly contributed by the land biospheric flux seasonality. Biospheric sink during postmonsoon is counterbalanced by emissions from fossil fuel burning. Biosphere and fossil fuel are major contributors in shaping the observed seasonal pattern with negligible seasonality in oceanic tracer due to its uniform flux patterns in the Indian Ocean. Mean diurnal pattern of CO₂ exhibits lower values during daytime (cleaner marine airmass) and higher values during nighttime (continental airmass) with deeper diurnal amplitude in the winter (~50 ppm) than in the summer (~31 ppm). Seasonal pattern in total column CO₂ from OCO-2 (Orbiting Carbon Observatory-2) is similar to the surface observations but shows nearly half of the observed seasonal amplitude. Long-term continuous measurements over distinct environments are desirable for further deepening the understanding of CO₂ variability, estimation of regional carbon budget and for climate mitigation policies.

Keywords: Carbon dioxide; In situ measurements; MIROC4-ACTM; Mesoscale circulation; OCO-2.