Fine particle pH and gas–particle phase partitioning of inorganic species in Pasadena, California, during the 2010 CalNex campaign
- Location
-
Deutsche Nationalbibliothek Frankfurt am Main
- Extent
-
Online-Ressource
- Language
-
Englisch
- Bibliographic citation
-
Fine particle pH and gas–particle phase partitioning of inorganic species in Pasadena, California, during the 2010 CalNex campaign ; volume:17 ; number:9 ; year:2017 ; pages:5703-5719
Atmospheric chemistry and physics ; 17, Heft 9 (2017), 5703-5719
- Creator
-
Guo, Hongyu
Liu, Jiumeng
Froyd, Karl D.
Roberts, James M.
Veres, Patrick R.
Hayes, Patrick L.
Jimenez, Jose L.
Nenes, Athanasios
Weber, Rodney J.
- DOI
-
10.5194/acp-17-5703-2017
- URN
-
urn:nbn:de:101:1-2017100917101
- Rights
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
- 15.08.2025, 7:33 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
- Guo, Hongyu
- Liu, Jiumeng
- Froyd, Karl D.
- Roberts, James M.
- Veres, Patrick R.
- Hayes, Patrick L.
- Jimenez, Jose L.
- Nenes, Athanasios
- Weber, Rodney J.
Other Objects (12)
Gas/particle partitioning of water-soluble organic aerosol in Atlanta
Modeling of the chemistry in oxidation flow reactors with high initial NO
Modeling of the chemistry in oxidation flow reactors with high initial NO
Parameterizing the competition between homogeneous and heterogeneous freezing in cirrus cloud formation – monodisperse ice nuclei
Droplet activation parameterization: the population-splitting concept revisited
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
Understanding the contributions of aerosol properties and parameterization discrepancies to droplet number variability in a global climate model
Cloud droplet activation: solubility revisited
Parameterizing the competition between homogeneous and heterogeneous freezing in ice cloud formation – polydisperse ice nuclei
High levels of ammonia do not raise fine particle pH sufficiently to yield nitrogen oxide-dominated sulfate production
Effectiveness of ammonia reduction on control of fine particle nitrate
Effectiveness of Ammonia Reduction on Control of Fine Particle Nitrate
Gas/particle partitioning of water-soluble organic aerosol in Atlanta
Modeling of the chemistry in oxidation flow reactors with high initial NO
Modeling of the chemistry in oxidation flow reactors with high initial NO
Parameterizing the competition between homogeneous and heterogeneous freezing in cirrus cloud formation – monodisperse ice nuclei
Droplet activation parameterization: the population-splitting concept revisited
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
Understanding the contributions of aerosol properties and parameterization discrepancies to droplet number variability in a global climate model
Cloud droplet activation: solubility revisited
Parameterizing the competition between homogeneous and heterogeneous freezing in ice cloud formation – polydisperse ice nuclei
High levels of ammonia do not raise fine particle pH sufficiently to yield nitrogen oxide-dominated sulfate production
Effectiveness of ammonia reduction on control of fine particle nitrate
Effectiveness of Ammonia Reduction on Control of Fine Particle Nitrate
Gas/particle partitioning of water-soluble organic aerosol in Atlanta
Modeling of the chemistry in oxidation flow reactors with high initial NO
Modeling of the chemistry in oxidation flow reactors with high initial NO
Parameterizing the competition between homogeneous and heterogeneous freezing in cirrus cloud formation – monodisperse ice nuclei
Droplet activation parameterization: the population-splitting concept revisited
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
Understanding the contributions of aerosol properties and parameterization discrepancies to droplet number variability in a global climate model
Cloud droplet activation: solubility revisited
Parameterizing the competition between homogeneous and heterogeneous freezing in ice cloud formation – polydisperse ice nuclei
High levels of ammonia do not raise fine particle pH sufficiently to yield nitrogen oxide-dominated sulfate production
Effectiveness of ammonia reduction on control of fine particle nitrate