Drilldown: BibEntryCargo

From CSDMS
BibEntryCargo > BibType: journalArticle & Editors : D.P. Ames; N.W.T. Quinn; A.E. Rizzoli; or Heaps, Norman S.; or Jorgensen, S.E.; or Rice, S.P.; Roy, A.G.; Rhoads, B.L.; or Solomon, S.; Qin, D.; Manning, M.; Chen, Z.; Marquis, M.; Averyt, K.B.; Tignor, M.; Miller, H.L.; or Tonnessen, K.A.; or Wiley or de Boer, P.L., et al. or None & Year: 2000 - 2009 & Journal : Ecological Modelling or Hydrology and Earth System Sciences or Journal of Coastal Research or Journal of Hydrology or Ocean Dynamics or Ocean Modelling or Water or Water Resources Research

Use the filters below to narrow your results.

BibType: (Click arrow to add another value)
Title:
4DVAR data assimilation in the Intra-Americas Sea with the Regional Ocean Modeling System (ROMS) (2) · Prediction of Storm Surges and Wind Waves on Coastal Highways in Hurricane-Prone Areas (2) · An intercomparison between finite difference and finite element (TELEMAC) approaches to modelling west coast of Britain tides (2) · An inter-comparison of tidal solutions computed with a range of unstructured grid models of the Irish and Celtic Sea Regions (2) · Surface mining and reclamation effects on flood response of watersheds in the central Appalachian Plateau region: SURFACE MINING EFFECTS ON FLOOD RESPONSE (2) · The benefit of high-resolution operational weather forecasts for flash flood warning (2) · The effect of wave–current interactions on the storm surge and inundation in Charleston Harbor during Hurricane Hugo 1989 (2) · Modeling suspended sediment discharge from the Waipaoa River system, New Zealand: The last 3000 years (2) · Can soil moisture be mapped onto the terrain? (2) · Treatment of unresolved islands and ice in wind wave models (2) · An unstructured-grid finite-volume surface wave model (FVCOM-SWAVE): Implementation, validations and applications (2) · SELFE: A semi-implicit Eulerian–Lagrangian finite-element model for cross-scale ocean circulation (2) · Influence of rainfall observation network on model calibration and application (2) · Wind-generated waves in Hurricane Juan (2) · Comparison of entrainment in overflows simulated by z-coordinate, isopycnal and non-hydrostatic models (2)
 
Journal: (Click arrow to add another value)
Booktitle:
Volume:
172 (15) · 44 (13) · 12 (11) · 13 (10) · 43 (10) · 59 (10) · 9 (9) · 220 (9) · 45 (9) · 42 (8) · 38 (8) · 11 (8) · 50 (7) · 4 (7) · 36 (7) · 8 (6) · 40 (6)
ISBN:
Note:
None (5) · Auto downloaded ref at: 2019-12-31 (35) · Auto downloaded ref at: 2020-06-05 (4) · Auto downloaded ref at: 2020-06-08 (1) · Auto downloaded ref at: 2020-06-10 (7) · Auto downloaded ref at: 2020-06-12 (17) · Auto downloaded ref at: 2020-06-14 (8) · Auto downloaded ref at: 2020-06-15 (8) · Auto downloaded ref at: 2020-06-16 (16) · Auto downloaded ref at: 2020-06-17 (2) · Auto downloaded ref at: 2020-06-19 (30) · Auto downloaded ref at: 2020-06-21 (1) · Auto downloaded ref at: 2020-06-22 (17) · Auto downloaded ref at: 2020-06-23 (22) · Auto downloaded ref at: 2020-06-24 (37) · Auto downloaded ref at: 2020-06-25 (6) · Auto downloaded ref at: 2020-06-26 (66) · Auto downloaded ref at: 2020-06-27 (10) · Auto downloaded ref at: 2020-06-28 (10) · Auto downloaded ref at: 2020-07-03 (38) · Auto downloaded ref at: 2020-07-15 (8) · Auto downloaded ref at: 2020-07-16 (5) · Auto downloaded ref at: 2021-01-11 (5) · Auto downloaded ref at: 2021-04-20 (1) · Auto downloaded ref at: 2021-04-21 (2) · Auto downloaded ref at: 2021-04-24 (1) · Auto downloaded ref at: 2022-02-16 (1) · Auto downloaded ref at: 2022-02-17 (3) · Auto downloaded ref at: 2022-02-18 (1) · Auto downloaded ref at: 2022-02-19 (2) · Auto downloaded ref at: 2022-02-21 (6) · Auto downloaded ref at: 2022-02-22 (3) · Auto downloaded ref at: 2023-07-06 (1) · Auto downloaded ref at: 2024-08-16 (1) · Auto downloaded ref at: 2024-08-17 (3) · Auto downloaded ref at: 2024-08-18 (1) · Auto downloaded ref at: 2024-08-29 (4) · Auto downloaded ref at: 2024-08-30 (2)

Showing below up to 250 results in range #1 to #250.

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

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