Drilldown: BibEntryCargo

From CSDMS
BibEntryCargo > Firstname : Anonymous; or Kirby, James T.; or Logan, Liz C.; Narayanan, Sri Hari Krishna; Greve, Ralf; Heimbach, Patrick;

Use the filters below to narrow your results.

Firstname: (Click arrow to add another value)
Title:
A general wave equation for waves over rippled beds (1) · A note on linear surface wave-current interaction over slowly varying topography (1) · Comment on “Analysis of an Extreme Weather 5 Event in a Hyper Arid Region Using WRF-Hydro Coupling, Station, and Satellite data” (1) · Higher-order approximations in the parabolic equation method for water waves (1) · Mitigation of Model Bias Influences on Wave Data Assimilation with Multiple Assimilation Systems Using WaveWatch III v5.16 and SWAN v41.20 (1) · On the gradual reflection of weakly nonlinear Stokes waves in regions with varying topography (1) · Open Boundary Condition in Parabolic Equation Method (1) · Parabolic Wave Computations in Non‐Orthogonal Coordinate Systems (1) · Rational approximations in the parabolic equation method for water waves (1) · Review For GMD: “Mitigation of Model Bias influence on wave Data assimilation with multiple Assimilation systems Using WaveWatch III v5.16 and SWAN v41.20” By Li and Zhang (1) · Review of Simulating barrier island response to sea-level rise with the barrier island and inlet environment (BRIE) model v1.0 (1) · Review: Solid research but unclear in critical parts (1) · SICOPOLIS-AD v1: an open-source adjoint modeling framework for ice sheet simulation enabled by the algorithmic differentiation tool OpenAD (2) · SICOPOLIS-AD: Quick-Start Manual: Revision 0.11 (1) · Sicopolis-AD: Quick-Start Manual (1) · Supplementary material to "SICOPOLIS-AD v1: an open-source adjoint modeling framework for ice sheet simulation enabled by the algorithmic differentiation tool OpenAD" (1)
Editors:
Booktitle:
Volume:
ISBN:

Showing below up to 17 results in range #1 to #17.

View (previous 250 | next 250) (20 | 50 | 100 | 250 | 500)


View (previous 250 | next 250) (20 | 50 | 100 | 250 | 500)