Measurements and modelling of I 2, IO, OIO, BrO and NO 3 in the mid-latitude marine boundary layer

Saiz-Lopez, A.; Shillito, J. A.; Coe, H.; Plane, J. M. C.

Time series observations of molecular iodine (I 2), iodine oxides (IO, OIO), bromine oxide (BrO), and the nitrate radical (NO 3) in the mid-latitude coastal marine boundary layer (MBL) are reported. Measurements were made using a new long-path DOAS instrument during a summertime campaign at Mace Head on the B3Π(0 +u)- X1Σ +g electronic transition between 535 and 575 nm. The I 2 mixing ratio was found to vary from below the detection limit (~5 ppt) up to a nighttime maximum of 93 ppt. Along with I 2, observations of IO, OIO and NO 3 were also made during the night. Surprisingly, IO and OIO were detected at mixing ratios up to 2.5 and 10.8 ppt, respectively. A model is employed to show that the reaction between I 2 and NO 3 is the likely nighttime source of these radicals. The BrO mixing ratio varied from below the detection limit at night (~1 ppt) to a maximum of 6 ppt in the first hours after sunrise. A bromine chemistry model is used to simulate the diurnal behaviour of the BrO radical, demonstrating the importance of halogen recycling through sea-salt aerosol. In the same campaign a zenith sky DOAS was employed to determine the column density variation of NO 3 as a function of solar zenith angle (SZA) during sunrise, from which vertical profiles of NO 3 through the troposphere were obtained. On several occasions a positive gradient of NO 3 was observed over the first 2 km, possibly due to dimethyl sulphide (DMS) removing NO 3 at the ocean surface.



Saiz-Lopez, A. / Shillito, J. A. / Coe, H. / et al: Measurements and modelling of I2, IO, OIO, BrO and NO3 in the mid-latitude marine boundary layer. 2006. Copernicus Publications.


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