Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements
| ISSN: |
1434-4483
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| Source: |
Springer Online Journal Archives 1860-2000
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| Topics: |
Geosciences
Physics
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| Notes: |
Summary Using existing physical parameterizations, a new mathematical model is formulated to diagnose the diurnal variation of the energy fluxes and temperature on the snow-free tundra surface at Princess Marie Bay, Ellesmere Island, Canada. The input to the model consists of three meteorological variables which can be readily measured by an automatic weather station: incoming short-wave radiation, windspeed and screen level temperature. The model is based on the one-dimensional heat conduction equation for unfrozen soil, with surface heat exchange by short- and long-wave radiation and by convection and evaporation. A permafrost surface is used as a lower boundary condition. The model is formulated and tuned using a series of data from the Princess Marie Bay site. It is then tested using a separate data set from the same site and an independent data set from a nearby site.
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| Type of Medium: |
Electronic Resource
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| URL: |
| _version_ | 1798297674523344898 |
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| autor | Szilder, K. Henry, G. H. R. Lozowski, E. P. Labine, C. |
| autorsonst | Szilder, K. Henry, G. H. R. Lozowski, E. P. Labine, C. |
| book_url | http://dx.doi.org/10.1007/BF00865162 |
| datenlieferant | nat_lic_papers |
| hauptsatz | hsatz_simple |
| identnr | NLM208209085 |
| issn | 1434-4483 |
| journal_name | Theoretical and applied climatology |
| materialart | 1 |
| notes | Summary Using existing physical parameterizations, a new mathematical model is formulated to diagnose the diurnal variation of the energy fluxes and temperature on the snow-free tundra surface at Princess Marie Bay, Ellesmere Island, Canada. The input to the model consists of three meteorological variables which can be readily measured by an automatic weather station: incoming short-wave radiation, windspeed and screen level temperature. The model is based on the one-dimensional heat conduction equation for unfrozen soil, with surface heat exchange by short- and long-wave radiation and by convection and evaporation. A permafrost surface is used as a lower boundary condition. The model is formulated and tuned using a series of data from the Princess Marie Bay site. It is then tested using a separate data set from the same site and an independent data set from a nearby site. |
| package_name | Springer |
| publikationsjahr_anzeige | 1996 |
| publikationsjahr_facette | 1996 |
| publikationsjahr_intervall | 8004:1995-1999 |
| publikationsjahr_sort | 1996 |
| publisher | Springer |
| reference | 54 (1996), S. 201-211 |
| search_space | articles |
| shingle_author_1 | Szilder, K. Henry, G. H. R. Lozowski, E. P. Labine, C. |
| shingle_author_2 | Szilder, K. Henry, G. H. R. Lozowski, E. P. Labine, C. |
| shingle_author_3 | Szilder, K. Henry, G. H. R. Lozowski, E. P. Labine, C. |
| shingle_author_4 | Szilder, K. Henry, G. H. R. Lozowski, E. P. Labine, C. |
| shingle_catch_all_1 | Szilder, K. Henry, G. H. R. Lozowski, E. P. Labine, C. Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements Summary Using existing physical parameterizations, a new mathematical model is formulated to diagnose the diurnal variation of the energy fluxes and temperature on the snow-free tundra surface at Princess Marie Bay, Ellesmere Island, Canada. The input to the model consists of three meteorological variables which can be readily measured by an automatic weather station: incoming short-wave radiation, windspeed and screen level temperature. The model is based on the one-dimensional heat conduction equation for unfrozen soil, with surface heat exchange by short- and long-wave radiation and by convection and evaporation. A permafrost surface is used as a lower boundary condition. The model is formulated and tuned using a series of data from the Princess Marie Bay site. It is then tested using a separate data set from the same site and an independent data set from a nearby site. 1434-4483 14344483 Springer |
| shingle_catch_all_2 | Szilder, K. Henry, G. H. R. Lozowski, E. P. Labine, C. Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements Summary Using existing physical parameterizations, a new mathematical model is formulated to diagnose the diurnal variation of the energy fluxes and temperature on the snow-free tundra surface at Princess Marie Bay, Ellesmere Island, Canada. The input to the model consists of three meteorological variables which can be readily measured by an automatic weather station: incoming short-wave radiation, windspeed and screen level temperature. The model is based on the one-dimensional heat conduction equation for unfrozen soil, with surface heat exchange by short- and long-wave radiation and by convection and evaporation. A permafrost surface is used as a lower boundary condition. The model is formulated and tuned using a series of data from the Princess Marie Bay site. It is then tested using a separate data set from the same site and an independent data set from a nearby site. 1434-4483 14344483 Springer |
| shingle_catch_all_3 | Szilder, K. Henry, G. H. R. Lozowski, E. P. Labine, C. Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements Summary Using existing physical parameterizations, a new mathematical model is formulated to diagnose the diurnal variation of the energy fluxes and temperature on the snow-free tundra surface at Princess Marie Bay, Ellesmere Island, Canada. The input to the model consists of three meteorological variables which can be readily measured by an automatic weather station: incoming short-wave radiation, windspeed and screen level temperature. The model is based on the one-dimensional heat conduction equation for unfrozen soil, with surface heat exchange by short- and long-wave radiation and by convection and evaporation. A permafrost surface is used as a lower boundary condition. The model is formulated and tuned using a series of data from the Princess Marie Bay site. It is then tested using a separate data set from the same site and an independent data set from a nearby site. 1434-4483 14344483 Springer |
| shingle_catch_all_4 | Szilder, K. Henry, G. H. R. Lozowski, E. P. Labine, C. Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements Summary Using existing physical parameterizations, a new mathematical model is formulated to diagnose the diurnal variation of the energy fluxes and temperature on the snow-free tundra surface at Princess Marie Bay, Ellesmere Island, Canada. The input to the model consists of three meteorological variables which can be readily measured by an automatic weather station: incoming short-wave radiation, windspeed and screen level temperature. The model is based on the one-dimensional heat conduction equation for unfrozen soil, with surface heat exchange by short- and long-wave radiation and by convection and evaporation. A permafrost surface is used as a lower boundary condition. The model is formulated and tuned using a series of data from the Princess Marie Bay site. It is then tested using a separate data set from the same site and an independent data set from a nearby site. 1434-4483 14344483 Springer |
| shingle_title_1 | Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements |
| shingle_title_2 | Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements |
| shingle_title_3 | Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements |
| shingle_title_4 | Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements |
| sigel_instance_filter | dkfz geomar wilbert ipn albert fhp |
| source_archive | Springer Online Journal Archives 1860-2000 |
| timestamp | 2024-05-06T10:11:45.236Z |
| titel | Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements |
| titel_suche | Diagnosing the diurnal surface energy balance over the summer tundra at Princess Marie Bay from simple short-period measurements |
| topic | TE-TZ U |
| uid | nat_lic_papers_NLM208209085 |