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First 300 results for ” W Sulistya”

1. Can we explain the observed methane variability after the Mount Pinatubo eruption?

   The CH4 growth rate in the atmosphere showed large variations after the Pinatubo eruption in June...

   N Bândă, M Krol, M van Weele, T van Noije, P Le Sager, T Röckmann | Status: published | Journal: Atmos. Chem. Phys. | Volume: 16 | Year: 2016 | First page: 195 | Last page: 214 | doi: 10.5194/acp-16-195-2016

   Publication

2. Curriculum vitae of the LOTOS–EUROS (v2.0) chemistry transport model

   The development and application of chemistry transport models has a long tradition. Within the Ne...

   Astrid M. M. Manders, John Douros, Henk Eskes, Peter van Velthoven | Status: published | Journal: Geoscientific Model Development | Volume: Volume 10, issue 11 | Year: 2017 | doi: https://doi.org/10.5194/gmd-10-4145-2017

   Publication

3. Coupling of the air quality model LOTOS-EUROS to the climate model RACMO

   Ozone and particulate matter have an adverse impact on the health of humans and other organisms. ...

   A Manders, B van Ulft, E van Meijgaard, M Schaap | Year: 2011

   Publication

4. Air pollution scenario over Pakistan: Characterization and ranking of extremely polluted cities using long-term concentrations of aerosols and trace gases.

   Pakistan ranks third in the world in terms of mortality attributable to air pollution, with aeros...

   Bilal, M., A. Mhawish, J.E. Nichol, Z. Qiu, M. Nazeer, Md. A. Ali, G. de Leeuw, R.C. Levy, Y. Wang, Y. Chen, L. Wang, Y. Shi, M.P. Bleiweiss, U. Mazhar, L. Atique, S. Ke | Journal: Remote Sensing of Environment | Year: 2021 | doi: 10.1016/j.rse.2021.112617

   Publication

5. Estimation of future discharges of the River Rhine in the SWURVE project

   The change in the flow regime of the river Rhine by the end of the 21st century was one of the ei...

   TA Buishand, G Lenderink | Year: 2004

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