Webbläsaren som du använder stöds inte av denna webbplats. Alla versioner av Internet Explorer stöds inte längre, av oss eller Microsoft (läs mer här: * https://www.microsoft.com/en-us/microsoft-365/windows/end-of-ie-support).

Var god och använd en modern webbläsare för att ta del av denna webbplats, som t.ex. nyaste versioner av Edge, Chrome, Firefox eller Safari osv.

Protrait Alex Vermeulen

Alex Vermeulen

Chef

Protrait Alex Vermeulen

Reassessing the variability in atmospheric H2 using the two-way nested TM5 model

Författare

  • G. Pieterse
  • M. C. Krol
  • A. M. Batenburg
  • C. A. M. Brenninkmeijer
  • M. E. Popa
  • S. O'Doherty
  • A. Grant
  • L. P. Steele
  • P. B. Krummel
  • R. L. Langenfelds
  • H. J. Wang
  • Alex Vermeulen
  • M. Schmidt
  • C. Yver
  • A. Jordan
  • A. Engel
  • R. E. Fisher
  • D. Lowry
  • E. G. Nisbet
  • S. Reimann
  • M. K. Vollmer
  • M. Steinbacher
  • S. Hammer
  • G. Forster
  • W. T. Sturges
  • T. Rockmann
Visa allt

Summary, in English

This work reassesses the global atmospheric budget of H2 with the TM5 model. The recent adjustment of the calibration scale for H2 translates into a change in the tropospheric burden. Furthermore, the ECMWF Reanalysis-Interim (ERA-Interim) data from the European Centre for Medium-Range Weather Forecasts (ECMWF) used in this study show slower vertical transport than the operational data used before. Consequently, more H2 is removed by deposition. The deposition parametrization is updated because significant deposition fluxes for snow, water, and vegetation surfaces were calculated in our previous study. Timescales of 1-2h are asserted for the transport of H2 through the canopies of densely vegetated regions. The global scale variability of H2 and [DH2] is well represented by the updated model. H2 is slightly overestimated in the Southern Hemisphere because too little H2 is removed by dry deposition to rainforests and savannahs. The variability in H2 over Europe is further investigated using a high-resolution model subdomain. It is shown that discrepancies between the model and the observations are mainly caused by the finite model resolution. The tropospheric burden is estimated at 165 +/- 8TgH2. The removal rates of H2 by deposition and photochemical oxidation are estimated at 53 +/- 4 and 23 +/- 2TgH2/yr, resulting in a tropospheric lifetime of 2.2 +/- 0.2year.

Publiceringsår

2013

Språk

Engelska

Sidor

3764-3780

Publikation/Tidskrift/Serie

Journal of Geophysical Research: Atmospheres

Volym

118

Issue

9

Dokumenttyp

Artikel i tidskrift

Förlag

Wiley-Blackwell

Ämne

  • Physical Geography

Nyckelord

  • tropospheric budget
  • Chemical Transport Model
  • molecular hydrogen
  • sources and sinks
  • hydrogen isotopes
  • dry deposition

Status

Published

ISBN/ISSN/Övrigt

  • ISSN: 2169-8996