Joint inference of groundwater–recharge and hydraulic–conductivity fields from head data using the ensemble Kalman filter
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Erschienen in
-
Joint inference of groundwater–recharge and hydraulic–conductivity fields from head data using the ensemble Kalman filter ; volume:20 ; number:1 ; year:2016 ; pages:555-569
Hydrology and earth system sciences ; 20, Heft 1 (2016), 555-569
- Urheber
-
Erdal, D.
Cirpka, O. A.
- DOI
-
10.5194/hess-20-555-2016
- URN
-
urn:nbn:de:101:1-201711056547
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
15.08.2025, 07:22 MESZ
Datenpartner
Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Beteiligte
- Erdal, D.
- Cirpka, O. A.
Ähnliche Objekte (12)
Full prediction of unsaturated hydraulic conductivity – comparison of four different capillary bundle models
Groundwater suitability recharge zones modelling – A GIS application
Groundwater recharge in Brandenburg is declining – but why?
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
Precipitation extremes on multiple time scales – Bartlett–Lewis Rectangular Pulse Model and Intensity–Duration–Frequency curves
Predicting groundwater recharge for varying landcover and climate conditions: – a global meta-study
M3A system (2000–2005) – operation and maintenance
Water yield following forest–grass–forest transitions
The long–term sea–level commitment from Antarctica
Friedrich Tamnau (1802–1879) – Mineraloge, Mineralsammler und Mäzen
HETerogeneous vectorized or Parallel (HETPv1.0): An updated inorganic heterogeneous chemistry solver for metastable state NH<sub>4</sub><sup>+</sup>–Na<sup>+</sup>–Ca<sup>2+</sup>–K<sup>+</sup>–Mg<sup>2+</sup>–SO<sub>4</sub><sup>2–</sup>–NO<sub>3</sub><sup>–</sup>–Cl<sup>–</sup> based on ISORROPIA II
CLUSTER–STAFF search coil magnetometer calibration – comparisons with FGM
Full prediction of unsaturated hydraulic conductivity – comparison of four different capillary bundle models
Groundwater suitability recharge zones modelling – A GIS application
Groundwater recharge in Brandenburg is declining – but why?
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
Precipitation extremes on multiple time scales – Bartlett–Lewis Rectangular Pulse Model and Intensity–Duration–Frequency curves
Predicting groundwater recharge for varying landcover and climate conditions: – a global meta-study
M3A system (2000–2005) – operation and maintenance
Water yield following forest–grass–forest transitions
The long–term sea–level commitment from Antarctica
Friedrich Tamnau (1802–1879) – Mineraloge, Mineralsammler und Mäzen
HETerogeneous vectorized or Parallel (HETPv1.0): An updated inorganic heterogeneous chemistry solver for metastable state NH<sub>4</sub><sup>+</sup>–Na<sup>+</sup>–Ca<sup>2+</sup>–K<sup>+</sup>–Mg<sup>2+</sup>–SO<sub>4</sub><sup>2–</sup>–NO<sub>3</sub><sup>–</sup>–Cl<sup>–</sup> based on ISORROPIA II
CLUSTER–STAFF search coil magnetometer calibration – comparisons with FGM
Full prediction of unsaturated hydraulic conductivity – comparison of four different capillary bundle models
Groundwater suitability recharge zones modelling – A GIS application
Groundwater recharge in Brandenburg is declining – but why?
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
Precipitation extremes on multiple time scales – Bartlett–Lewis Rectangular Pulse Model and Intensity–Duration–Frequency curves
Predicting groundwater recharge for varying landcover and climate conditions: – a global meta-study
M3A system (2000–2005) – operation and maintenance
Water yield following forest–grass–forest transitions
The long–term sea–level commitment from Antarctica
Friedrich Tamnau (1802–1879) – Mineraloge, Mineralsammler und Mäzen
HETerogeneous vectorized or Parallel (HETPv1.0): An updated inorganic heterogeneous chemistry solver for metastable state NH<sub>4</sub><sup>+</sup>–Na<sup>+</sup>–Ca<sup>2+</sup>–K<sup>+</sup>–Mg<sup>2+</sup>–SO<sub>4</sub><sup>2–</sup>–NO<sub>3</sub><sup>–</sup>–Cl<sup>–</sup> based on ISORROPIA II