Ice-nucleating particle concentration impacts cloud properties over Dronning Maud Land, East Antarctica, in COSMO-CLM2

zu Verbundenen Objekten

Standort: Deutsche Nationalbibliothek Frankfurt am Main

Umfang: Online-Ressource

Sprache: Englisch

Erschienen in: Ice-nucleating particle concentration impacts cloud properties over Dronning Maud Land, East Antarctica, in COSMO-CLM² ; day:27 ; month:05 ; year:2024 ; pages:1-24 ; extent:24
EGUsphere ; (27.05.2024), 1-24 (gesamt 24)

Urheber: Sauerland, Florian
Souverijns, Niels
Possner, Anna
Wex, Heike
Van Overmeiren, Preben
Mangold, Alexander
Van Weverberg, Kwinten
van Lipzig, Nicole

DOI: 10.5194/egusphere-2024-1341

URN: urn:nbn:de:101:1-2405300426053.689546383710

Rechteinformation: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Letzte Aktualisierung: 05.11.2025, 15:09 MEZ

Datenpartner

Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.

Original beim Datenpartner anzeigen

Beteiligte

Sauerland, Florian
Souverijns, Niels
Possner, Anna
Wex, Heike
Van Overmeiren, Preben
Mangold, Alexander
Van Weverberg, Kwinten
van Lipzig, Nicole

Ähnliche Objekte (12)

Soils rich in biological ice-nucleating particles abound in ice-nucleating macromolecules likely produced by fungi

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: FeII, CoII, NiII, CuII und CuII)

Hochschulschrift

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: FeII, CoII, NiII, CuII und CuII)

Ice-Nucleating Particles Near Two Major Dust Source Regions

Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

HETerogeneous vectorized or Parallel (HETPv1.0): an updated inorganic heterogeneous chemistry solver for the metastable-state NH4+–Na+–Ca2+–K+–Mg2+–SO42−–NO3−–Cl−–H2O system based on ISORROPIA II

HETerogeneous vectorized or Parallel (HETPv1.0): an updated inorganic heterogeneous chemistry solver for the metastable-state NH4+–Na+–Ca2+–K+–Mg2+–SO42−–NO3−–Cl−–H2O system based on ISORROPIA II

HETerogeneous vectorized or Parallel (HETPv1.0): An updated inorganic heterogeneous chemistry solver for metastable state NH4+–Na+–Ca2+–K+–Mg2+–SO42––NO3––Cl– based on ISORROPIA II

HETerogeneous vectorized or Parallel (HETPv1.0): An updated inorganic heterogeneous chemistry solver for metastable state NH4+–Na+–Ca2+–K+–Mg2+–SO42––NO3––Cl– based on ISORROPIA II

Precise dating of deglacial Laptev Sea sediments via 14C and authigenic 10Be/9Be – assessing local 14C reservoir ages

Precise dating of deglacial Laptev Sea sediments via 14C and authigenic 10Be/9Be – assessing local 14C reservoir ages

Insights into Protein Dynamics from 15N-1H HSQC

Insights into Protein Dynamics from 15N-1H HSQC

Condensation/immersion mode ice-nucleating particles in a boreal environment

Active thermokarst regions contain rich sources of ice-nucleating particles

Hochschulschrift

Airborne-based geophysical investigation in Dronning Maud Land, Antarctica

Reaction dynamics of P (4S) + O2(X 3Σ-) → O (3P) + PO (X 2Π) on a global CHIPR potential energy surface of PO2(X 2A1): implication for atmospheric modelling

Reaction dynamics of P (4S) + O2(X 3Σ-) → O (3P) + PO (X 2Π) on a global CHIPR potential energy surface of PO2(X 2A1): implication for atmospheric modelling

Soils rich in biological ice-nucleating particles abound in ice-nucleating macromolecules likely produced by fungi

Hochschulschrift

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: FeII, CoII, NiII, CuII und CuII)

Ice-Nucleating Particles Near Two Major Dust Source Regions

Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

HETerogeneous vectorized or Parallel (HETPv1.0): an updated inorganic heterogeneous chemistry solver for the metastable-state NH4+–Na+–Ca2+–K+–Mg2+–SO42−–NO3−–Cl−–H2O system based on ISORROPIA II

HETerogeneous vectorized or Parallel (HETPv1.0): An updated inorganic heterogeneous chemistry solver for metastable state NH4+–Na+–Ca2+–K+–Mg2+–SO42––NO3––Cl– based on ISORROPIA II

Precise dating of deglacial Laptev Sea sediments via 14C and authigenic 10Be/9Be – assessing local 14C reservoir ages

Insights into Protein Dynamics from 15N-1H HSQC

Condensation/immersion mode ice-nucleating particles in a boreal environment

Active thermokarst regions contain rich sources of ice-nucleating particles

Hochschulschrift

Airborne-based geophysical investigation in Dronning Maud Land, Antarctica

Reaction dynamics of P (4S) + O2(X 3Σ-) → O (3P) + PO (X 2Π) on a global CHIPR potential energy surface of PO2(X 2A1): implication for atmospheric modelling

Soils rich in biological ice-nucleating particles abound in ice-nucleating macromolecules likely produced by fungi

Hochschulschrift

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: FeII, CoII, NiII, CuII und CuII)

Ice-Nucleating Particles Near Two Major Dust Source Regions

Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

HETerogeneous vectorized or Parallel (HETPv1.0): an updated inorganic heterogeneous chemistry solver for the metastable-state NH4+–Na+–Ca2+–K+–Mg2+–SO42−–NO3−–Cl−–H2O system based on ISORROPIA II

HETerogeneous vectorized or Parallel (HETPv1.0): An updated inorganic heterogeneous chemistry solver for metastable state NH4+–Na+–Ca2+–K+–Mg2+–SO42––NO3––Cl– based on ISORROPIA II

Precise dating of deglacial Laptev Sea sediments via 14C and authigenic 10Be/9Be – assessing local 14C reservoir ages

Insights into Protein Dynamics from 15N-1H HSQC

Condensation/immersion mode ice-nucleating particles in a boreal environment

Active thermokarst regions contain rich sources of ice-nucleating particles

Hochschulschrift

Airborne-based geophysical investigation in Dronning Maud Land, Antarctica

Reaction dynamics of P (4S) + O2(X 3Σ-) → O (3P) + PO (X 2Π) on a global CHIPR potential energy surface of PO2(X 2A1): implication for atmospheric modelling

Informationen zur Registrierung von Kultur- und Wissenseinrichtungen finden Sie hier.

Felder mit * müssen ausgefüllt werden.

Benutzername*

Bitte geben Sie Ihren Benutzernamen ein

E-Mail*

Bitte geben Sie Ihre E-Mail ein

Bitte füllen Sie dieses Feld nicht aus

Vorname

Nachname

Passwort*

Bitte geben Sie Ihr Passwort ein

Passwort bestätigen*

Bitte geben Sie das gleiche Passwort ein

Ich habe die Nutzungsbedingungen und die Datenschutzerklärung zur Erhebung persönlicher Daten gelesen und stimme ihnen zu. *

Dieses Feld ist ein Pflichtfeld.

Ich möchte den Newsletter der Deutschen Digitalen Bibliothek abonnieren. Siehe Informationen zum Newsletter-Abonnement.

Benutzerkonto angelegt

Ihr „Meine DDB“-Konto wurde erfolgreich angelegt. Bevor Sie sich in Ihrem Konto anmelden können, müssen Sie auf den Bestätigungslink in der Nachricht klicken, die wir gerade an die von Ihnen angegebene E-Mail-Adresse geschickt haben

Deutschlands Kulturerbe digital

Ice-nucleating particle concentration impacts cloud properties over Dronning Maud Land, East Antarctica, in COSMO-CLM<sup>2</sup>

Datenpartner

Beteiligte

Ähnliche Objekte (12)

Soils rich in biological ice-nucleating particles abound in ice-nucleating macromolecules likely produced by fungi

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Ice-Nucleating Particles Near Two Major Dust Source Regions

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

Condensation/immersion mode ice-nucleating particles in a boreal environment

Active thermokarst regions contain rich sources of ice-nucleating particles

Airborne-based geophysical investigation in Dronning Maud Land, Antarctica

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Soils rich in biological ice-nucleating particles abound in ice-nucleating macromolecules likely produced by fungi

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Ice-Nucleating Particles Near Two Major Dust Source Regions

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

Condensation/immersion mode ice-nucleating particles in a boreal environment

Active thermokarst regions contain rich sources of ice-nucleating particles

Airborne-based geophysical investigation in Dronning Maud Land, Antarctica

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Soils rich in biological ice-nucleating particles abound in ice-nucleating macromolecules likely produced by fungi

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Ice-Nucleating Particles Near Two Major Dust Source Regions

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

Condensation/immersion mode ice-nucleating particles in a boreal environment

Active thermokarst regions contain rich sources of ice-nucleating particles

Airborne-based geophysical investigation in Dronning Maud Land, Antarctica

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Ice-nucleating particle concentration impacts cloud properties over Dronning Maud Land, East Antarctica, in COSMO-CLM<sup>2</sup>

Angaben zum Objekt

Verweise und Beziehungen

Beteiligte, Orts- und Zeitangaben

Weitere Informationen

Datenpartner

Beteiligte

Ähnliche Objekte (12)

Soils rich in biological ice-nucleating particles abound in ice-nucleating macromolecules likely produced by fungi

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Ice-Nucleating Particles Near Two Major Dust Source Regions

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

Condensation/immersion mode ice-nucleating particles in a boreal environment

Active thermokarst regions contain rich sources of ice-nucleating particles

Airborne-based geophysical investigation in Dronning Maud Land, Antarctica

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>&Sigma;<sup>-</sup>) &rarr; O (<sup>3</sup>P) + PO (X <sup>2</sup>&Pi;) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Soils rich in biological ice-nucleating particles abound in ice-nucleating macromolecules likely produced by fungi

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Ice-Nucleating Particles Near Two Major Dust Source Regions

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

Condensation/immersion mode ice-nucleating particles in a boreal environment

Active thermokarst regions contain rich sources of ice-nucleating particles

Airborne-based geophysical investigation in Dronning Maud Land, Antarctica

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>&Sigma;<sup>-</sup>) &rarr; O (<sup>3</sup>P) + PO (X <sup>2</sup>&Pi;) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Soils rich in biological ice-nucleating particles abound in ice-nucleating macromolecules likely produced by fungi

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Ice-Nucleating Particles Near Two Major Dust Source Regions

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

Condensation/immersion mode ice-nucleating particles in a boreal environment

Active thermokarst regions contain rich sources of ice-nucleating particles

Airborne-based geophysical investigation in Dronning Maud Land, Antarctica

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>&Sigma;<sup>-</sup>) &rarr; O (<sup>3</sup>P) + PO (X <sup>2</sup>&Pi;) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Verbundene Objekte

Passwort zurücksetzen

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling