Estimating the contribution of bromoform to stratospheric bromine and its relation to dehydration in the tropical tropopause layer

  • B. - M. Sinnhuber, I. Folkins
  • Published 2006


The contribution of bromoform to the stratospheric bromine loading is estimated using the onedimensional tropical mean model of Folkins and Martin (2005), which is constrained by observed mean profiles of temperature and humidity. In order to reach the stratosphere, bromoform needs to be lifted by deep convection into the tropical tropopause layer (TTL… (More)


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