Mark Žagar
Biographic Data
| ID | 6016397 |
|---|---|
| NAME | Mark Žagar |
| GIVEN NAMES | Mark |
| FAMILY NAME | Žagar |
| SIGNATURE | ŽAGAR M |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2004 |
| LATEST PUBLICATION YEAR | 2004 |
| H-INDEX | 0 |
Model Simulations of the Arctic Atmospheric Boundary Layer from the SHEBA Year
We present Arctic atmospheric boundary-layer modeling with a regional model COAMPS, for the Surface Heat Budget of the Arctic Ocean (SHEBA) experiment. Model results are compared to soundings, near-surface measurements and forecasts from the ECMWF model. The near-surface temperature is often too high in winter, except in shorter periods when the boundary layer was cloud-capped and well-mixed due to cloud-top cooling. Temperatures are slightly too…
Model Simulations of the Arctic Atmospheric Boundary Layer from the SHEBA Year
We present Arctic atmospheric boundary-layer modeling with a regional model COAMPSTM, for the Surface Heat Budget of the Arctic Ocean (SHEBA) experiment. Model results are compared to soundings, near-surface measurements and forecasts from the ECMWF model. The near-surface temperature is often too high in winter, except in shorter periods when the boundary layer was cloud-capped and well-mixed due to cloud-top cooling. Temperatures are slightly t…
No prominent works on this page.
Model Simulations of the Arctic Atmospheric Boundary Layer from the SHEBA Year
We present Arctic atmospheric boundary-layer modeling with a regional model COAMPS, for the Surface Heat Budget of the Arctic Ocean (SHEBA) experiment. Model results are compared to soundings, near-surface measurements and forecasts from the ECMWF model. The near-surface temperature is often too high in winter, except in shorter periods when the boundary layer was cloud-capped and well-mixed due to cloud-top cooling. Temperatures are slightly too…
Model Simulations of the Arctic Atmospheric Boundary Layer from the SHEBA Year
We present Arctic atmospheric boundary-layer modeling with a regional model COAMPSTM, for the Surface Heat Budget of the Arctic Ocean (SHEBA) experiment. Model results are compared to soundings, near-surface measurements and forecasts from the ECMWF model. The near-surface temperature is often too high in winter, except in shorter periods when the boundary layer was cloud-capped and well-mixed due to cloud-top cooling. Temperatures are slightly t…
Arctic and Antarctic ice dynamics (2 works) · Atmospheric sciences (2 works) · Boundary layer (2 works) · Climate change and permafrost (2 works) · Climatology (2 works) · Environmental Science (2 works) · Geology (2 works) · Mechanics (2 works) · Meteorology (2 works) · Physics (2 works)