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Mark Žagar

Biographic Data

ID6016397
NAMEMark Žagar
GIVEN NAMESMark
FAMILY NAMEŽagar
SIGNATUREŽAGAR M
VERIFIEDNo
TOTAL WORKS2
TOTAL CITATIONS0
WORKS AS AUTHOR2
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2004
LATEST PUBLICATION YEAR2004
H-INDEX0
  • Model Simulations of the Arctic Atmospheric Boundary Layer from the SHEBA Year

    Michael Tjernström, Mark Žagar et al.•ARTICLE•AMBIO•2004•References: 15

    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

    Michael Tjernström, Mark Žagar et al.•ARTICLE•AMBIO•2004

    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

    Michael Tjernström, Mark Žagar et al.•ARTICLE•AMBIO•2004•References: 15

    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

    Michael Tjernström, Mark Žagar et al.•ARTICLE•AMBIO•2004

    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)

Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae