- Location
-
Deutsche Nationalbibliothek Frankfurt am Main
- Extent
-
Online-Ressource
- Language
-
Englisch
- Bibliographic citation
-
Understanding nitrate formation in a world with less sulfate ; volume:18 ; number:17 ; year:2018 ; pages:12765-12775
Atmospheric chemistry and physics ; 18, Heft 17 (2018), 12765-12775
- Creator
- DOI
-
10.5194/acp-18-12765-2018
- URN
-
urn:nbn:de:101:1-2019021403595154398893
- Rights
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
- 14.08.2025, 10:48 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Vasilakos, Petros
- Russel, Armistead G.
- Weber, Rodney
- Nenes, Athanasios
Other Objects (12)
Understanding nitrate formation in a world with less sulfate
Understanding the contributions of aerosol properties and parameterization discrepancies to droplet number variability in a global climate model
The underappreciated role of nonvolatile cations on aerosol ammonium-sulfate molar ratios
Droplet activation parameterization: the population-splitting concept revisited
Cloud droplet activation: solubility revisited
Parameterizing the competition between homogeneous and heterogeneous freezing in ice cloud formation – polydisperse ice nuclei
ISORROPIA II: a computationally efficient thermodynamic equilibrium model for K + –Ca 2+ –Mg 2+ –NH 4 + –Na + –SO 4 2− –NO 3 − –Cl − –H 2 O aerosols
Parameterizing the competition between homogeneous and heterogeneous freezing in cirrus cloud formation – monodisperse ice nuclei
Aerosol pH and liquid water content determine when particulate matter is sensitive to ammonia and nitrate availability
High levels of ammonia do not raise fine particle pH sufficiently to yield nitrogen oxide-dominated sulfate production
Understanding cirrus ice crystal number variability for different heterogeneous ice nucleation spectra
Ammonium nitrate evaporation and nitric acid condensation in DMT CCN counters
Understanding nitrate formation in a world with less sulfate
Understanding the contributions of aerosol properties and parameterization discrepancies to droplet number variability in a global climate model
The underappreciated role of nonvolatile cations on aerosol ammonium-sulfate molar ratios
Droplet activation parameterization: the population-splitting concept revisited
Cloud droplet activation: solubility revisited
Parameterizing the competition between homogeneous and heterogeneous freezing in ice cloud formation – polydisperse ice nuclei
ISORROPIA II: a computationally efficient thermodynamic equilibrium model for K + –Ca 2+ –Mg 2+ –NH 4 + –Na + –SO 4 2− –NO 3 − –Cl − –H 2 O aerosols
Parameterizing the competition between homogeneous and heterogeneous freezing in cirrus cloud formation – monodisperse ice nuclei
Aerosol pH and liquid water content determine when particulate matter is sensitive to ammonia and nitrate availability
High levels of ammonia do not raise fine particle pH sufficiently to yield nitrogen oxide-dominated sulfate production
Understanding cirrus ice crystal number variability for different heterogeneous ice nucleation spectra
Ammonium nitrate evaporation and nitric acid condensation in DMT CCN counters
Understanding nitrate formation in a world with less sulfate
Understanding the contributions of aerosol properties and parameterization discrepancies to droplet number variability in a global climate model
The underappreciated role of nonvolatile cations on aerosol ammonium-sulfate molar ratios
Droplet activation parameterization: the population-splitting concept revisited
Cloud droplet activation: solubility revisited
Parameterizing the competition between homogeneous and heterogeneous freezing in ice cloud formation – polydisperse ice nuclei
ISORROPIA II: a computationally efficient thermodynamic equilibrium model for K + –Ca 2+ –Mg 2+ –NH 4 + –Na + –SO 4 2− –NO 3 − –Cl − –H 2 O aerosols
Parameterizing the competition between homogeneous and heterogeneous freezing in cirrus cloud formation – monodisperse ice nuclei
Aerosol pH and liquid water content determine when particulate matter is sensitive to ammonia and nitrate availability
High levels of ammonia do not raise fine particle pH sufficiently to yield nitrogen oxide-dominated sulfate production
Understanding cirrus ice crystal number variability for different heterogeneous ice nucleation spectra