Atmospheric gas-phase composition over the Indian Ocean

Type Article
Date 2022-05
Language English
Author(s) Tegtmeier Susann1, Marandino Christa2, Jia Yue1, Quack Birgit2, Mahajan Anoop S.3
Affiliation(s) 1 : Institute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, Canada
2 : Biogeochemistry Research Division, GEOMAR Helmholtz Centre for Ocean Research Kiel, 24105 Kiel, Germany​​​​​​​
3 : Center for Climate Change Research, Indian Institute of Tropical Meteorology, Pune, 411016, India
Source Atmospheric Chemistry And Physics (1680-7316) (Copernicus Gesellschaft Mbh), 2022-05 , Vol. 22 , N. 10 , P. 6625-6676
DOI 10.5194/acp-22-6625-2022
WOS© Times Cited 3
Note Special issue : Understanding the Indian Ocean system: past, present and future (BG/ACP/OS/SE inter-journal SI) Editor(s): Rolf Müller Special issue jointly organized between Biogeosciences, Atmospheric Chemistry and Physics, Ocean Science, and Solid Earth
Abstract

The Indian Ocean is coupled to atmospheric dynamics and chemical composition via several unique mechanisms, such as the seasonally varying monsoon circulation. During the winter monsoon season, high pollution levels are regularly observed over the entire northern Indian Ocean, while during the summer monsoon, clean air dominates the atmospheric composition, leading to distinct chemical regimes. The changing atmospheric composition over the Indian Ocean can interact with oceanic biogeochemical cycles and impact marine ecosystems, resulting in potential climate feedbacks. Here, we review current progress in detecting and understanding atmospheric gas-phase composition over the Indian Ocean and its local and global impacts. The review considers results from recent Indian Ocean ship campaigns, satellite measurements, station data, and information on continental and oceanic trace gas emissions. The distribution of all major pollutants and greenhouse gases shows pronounced differences between the landmass source regions and the Indian Ocean, with strong gradients over the coastal areas. Surface pollution and ozone are highest during the winter monsoon over the Bay of Bengal and the Arabian Sea coastal waters due to air mass advection from the Indo-Gangetic Plain and continental outflow from Southeast Asia. We observe, however, that unusual types of wind patterns can lead to pronounced deviations of the typical trace gas distributions. For example, the ozone distribution maxima shift to different regions under wind scenarios that differ from the regular seasonal transport patterns. The distribution of greenhouse gases over the Indian Ocean shows many similarities when compared to the pollution fields, but also some differences of the latitudinal and seasonal variations resulting from their long lifetimes and biogenic sources. Mixing ratios of greenhouse gases such as methane show positive trends over the Indian Ocean, but long-term changes in pollution and ozone due to changing emissions and transport patterns require further investigation. Although we know that changing atmospheric composition and perturbations within the Indian Ocean affect each other, the impacts of atmospheric pollution on oceanic biogeochemistry and trace gas cycling are severely understudied. We highlight potential mechanisms, future research topics, and observational requirements that need to be explored in order to fully understand such interactions and feedbacks in the Indian Ocean region.

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