4.6 Article

Spatial and Temporal Variability of Iodine in Aerosol

期刊

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020JD034410

关键词

aerosol composition; atmospheric iodine; iodine sources

资金

  1. State Agency for Research of the Spanish MCIU through the Center of Excellence Severo Ochoa award [SEV-2017-0709]
  2. Ramon y Cajal Program [RYC-2016-19,570]
  3. European Research Council Executive Agency under the European Union's Horizon 2020 Research and Innovation program [ERC-2016-COG 726349]
  4. ANPCyT [PICT 2015-0714]
  5. UNCuyo [SeCTyP M032/3853]
  6. UTN [PID 4920-194/2018]

向作者/读者索取更多资源

This study compiled and homogenized a dataset of aerosol iodine field observations from 1963 to 2018, showing a close to linear relationship between soluble and total iodine in aerosol. The data set revealed distinct latitudinal dependence of aerosol iodine, with higher concentrations in the Northern Hemisphere tropics. New observations from Antarctica demonstrated a seasonal variation of iodine in aerosol similar to that in the Arctic.
In this work, we describe the compilation and homogenization of an extensive data set of aerosol iodine field observations in the period between 1963 and 2018 and we discuss its spatial and temporal dependences by comparison with CAM-Chem model simulations. A close to linear relationship between soluble and total iodine in aerosol is found (similar to 80% aerosol iodine is soluble), which enables converting a large subset of measurements of soluble iodine into total iodine. The resulting data set shows a distinct latitudinal dependence, with an enhancement toward the Northern Hemisphere (NH) tropics and lower values toward the poles. This behavior, which has been predicted by atmospheric models to depend on the global distribution of the main oceanic iodine source (which in turn depends on the reaction of ozone with aqueous iodide on the sea water-air interface, generating gas-phase I-2 and HOI), is confirmed here by field observations for the first time. Longitudinally, there is some indication of a wave-one profile in the tropics, which peaks in the Atlantic and shows a minimum in the Pacific. New data from Antarctica show that the south polar seasonal variation of iodine in aerosol mirrors that observed previously in the Arctic, with two equinoctial maxima and the dominant maximum occurring in spring. While no clear seasonal variability is observed in NH middle latitudes, there is an indication of different seasonal cycles in the NH tropical Atlantic and Pacific. Long-term trends cannot be unambiguously established as a result of inhomogeneous time and spatial coverage and analytical methods.

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