Theoretical determination of the surface energy balance and thermal regimes of bare soils
Abstract An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determin...
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| Autor*in: |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1985 |
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| Umfang: |
21 |
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| Reproduktion: |
Springer Online Journal Archives 1860-2002 |
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| Übergeordnetes Werk: |
in: Boundary layer meteorology - 1970, 33(1985) vom: Apr., Seite 313-333 |
| Übergeordnetes Werk: |
volume:33 ; year:1985 ; month:04 ; pages:313-333 ; extent:21 |
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NLEJ193485761 |
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| 245 | 1 | 0 | |a Theoretical determination of the surface energy balance and thermal regimes of bare soils |
| 264 | 1 | |c 1985 | |
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| 520 | |a Abstract An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determined using a surface resistance to vapour flow. Fourier superposition is used to represent nonsinusoidal variations in time due to effects such as variable cloud cover. The theory is in acceptable agreement with micrometeorological measurements made at two bare soil sites of contrasting surface bulk density. It is concluded that the surface resistance model for evaporation is applicable to bare soils which remain wet at depth, particularly if their surface is loosened. The theory is used to predict the diurnal thermal regimes of saturated and dry sand, loam, and peat soils. | ||
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| 700 | 1 | |a Novak, M. D. |4 oth | |
| 700 | 1 | |a Black, T. A. |4 oth | |
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(DE-627)NLEJ193485761 DE-627 ger DE-627 rakwb eng Theoretical determination of the surface energy balance and thermal regimes of bare soils 1985 21 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determined using a surface resistance to vapour flow. Fourier superposition is used to represent nonsinusoidal variations in time due to effects such as variable cloud cover. The theory is in acceptable agreement with micrometeorological measurements made at two bare soil sites of contrasting surface bulk density. It is concluded that the surface resistance model for evaporation is applicable to bare soils which remain wet at depth, particularly if their surface is loosened. The theory is used to predict the diurnal thermal regimes of saturated and dry sand, loam, and peat soils. Springer Online Journal Archives 1860-2002 Novak, M. D. oth Black, T. A. oth in Boundary layer meteorology 1970 33(1985) vom: Apr., Seite 313-333 (DE-627)NLEJ18899307X (DE-600)1477639-x 1573-1472 nnns volume:33 year:1985 month:04 pages:313-333 extent:21 http://dx.doi.org/10.1007/BF00116682 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 33 1985 4 313-333 21 |
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(DE-627)NLEJ193485761 DE-627 ger DE-627 rakwb eng Theoretical determination of the surface energy balance and thermal regimes of bare soils 1985 21 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determined using a surface resistance to vapour flow. Fourier superposition is used to represent nonsinusoidal variations in time due to effects such as variable cloud cover. The theory is in acceptable agreement with micrometeorological measurements made at two bare soil sites of contrasting surface bulk density. It is concluded that the surface resistance model for evaporation is applicable to bare soils which remain wet at depth, particularly if their surface is loosened. The theory is used to predict the diurnal thermal regimes of saturated and dry sand, loam, and peat soils. Springer Online Journal Archives 1860-2002 Novak, M. D. oth Black, T. A. oth in Boundary layer meteorology 1970 33(1985) vom: Apr., Seite 313-333 (DE-627)NLEJ18899307X (DE-600)1477639-x 1573-1472 nnns volume:33 year:1985 month:04 pages:313-333 extent:21 http://dx.doi.org/10.1007/BF00116682 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 33 1985 4 313-333 21 |
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(DE-627)NLEJ193485761 DE-627 ger DE-627 rakwb eng Theoretical determination of the surface energy balance and thermal regimes of bare soils 1985 21 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determined using a surface resistance to vapour flow. Fourier superposition is used to represent nonsinusoidal variations in time due to effects such as variable cloud cover. The theory is in acceptable agreement with micrometeorological measurements made at two bare soil sites of contrasting surface bulk density. It is concluded that the surface resistance model for evaporation is applicable to bare soils which remain wet at depth, particularly if their surface is loosened. The theory is used to predict the diurnal thermal regimes of saturated and dry sand, loam, and peat soils. Springer Online Journal Archives 1860-2002 Novak, M. D. oth Black, T. A. oth in Boundary layer meteorology 1970 33(1985) vom: Apr., Seite 313-333 (DE-627)NLEJ18899307X (DE-600)1477639-x 1573-1472 nnns volume:33 year:1985 month:04 pages:313-333 extent:21 http://dx.doi.org/10.1007/BF00116682 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 33 1985 4 313-333 21 |
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(DE-627)NLEJ193485761 DE-627 ger DE-627 rakwb eng Theoretical determination of the surface energy balance and thermal regimes of bare soils 1985 21 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determined using a surface resistance to vapour flow. Fourier superposition is used to represent nonsinusoidal variations in time due to effects such as variable cloud cover. The theory is in acceptable agreement with micrometeorological measurements made at two bare soil sites of contrasting surface bulk density. It is concluded that the surface resistance model for evaporation is applicable to bare soils which remain wet at depth, particularly if their surface is loosened. The theory is used to predict the diurnal thermal regimes of saturated and dry sand, loam, and peat soils. Springer Online Journal Archives 1860-2002 Novak, M. D. oth Black, T. A. oth in Boundary layer meteorology 1970 33(1985) vom: Apr., Seite 313-333 (DE-627)NLEJ18899307X (DE-600)1477639-x 1573-1472 nnns volume:33 year:1985 month:04 pages:313-333 extent:21 http://dx.doi.org/10.1007/BF00116682 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 33 1985 4 313-333 21 |
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(DE-627)NLEJ193485761 DE-627 ger DE-627 rakwb eng Theoretical determination of the surface energy balance and thermal regimes of bare soils 1985 21 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determined using a surface resistance to vapour flow. Fourier superposition is used to represent nonsinusoidal variations in time due to effects such as variable cloud cover. The theory is in acceptable agreement with micrometeorological measurements made at two bare soil sites of contrasting surface bulk density. It is concluded that the surface resistance model for evaporation is applicable to bare soils which remain wet at depth, particularly if their surface is loosened. The theory is used to predict the diurnal thermal regimes of saturated and dry sand, loam, and peat soils. Springer Online Journal Archives 1860-2002 Novak, M. D. oth Black, T. A. oth in Boundary layer meteorology 1970 33(1985) vom: Apr., Seite 313-333 (DE-627)NLEJ18899307X (DE-600)1477639-x 1573-1472 nnns volume:33 year:1985 month:04 pages:313-333 extent:21 http://dx.doi.org/10.1007/BF00116682 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 33 1985 4 313-333 21 |
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theoretical determination of the surface energy balance and thermal regimes of bare soils |
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Theoretical determination of the surface energy balance and thermal regimes of bare soils |
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Abstract An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determined using a surface resistance to vapour flow. Fourier superposition is used to represent nonsinusoidal variations in time due to effects such as variable cloud cover. The theory is in acceptable agreement with micrometeorological measurements made at two bare soil sites of contrasting surface bulk density. It is concluded that the surface resistance model for evaporation is applicable to bare soils which remain wet at depth, particularly if their surface is loosened. The theory is used to predict the diurnal thermal regimes of saturated and dry sand, loam, and peat soils. |
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Abstract An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determined using a surface resistance to vapour flow. Fourier superposition is used to represent nonsinusoidal variations in time due to effects such as variable cloud cover. The theory is in acceptable agreement with micrometeorological measurements made at two bare soil sites of contrasting surface bulk density. It is concluded that the surface resistance model for evaporation is applicable to bare soils which remain wet at depth, particularly if their surface is loosened. The theory is used to predict the diurnal thermal regimes of saturated and dry sand, loam, and peat soils. |
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Abstract An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determined using a surface resistance to vapour flow. Fourier superposition is used to represent nonsinusoidal variations in time due to effects such as variable cloud cover. The theory is in acceptable agreement with micrometeorological measurements made at two bare soil sites of contrasting surface bulk density. It is concluded that the surface resistance model for evaporation is applicable to bare soils which remain wet at depth, particularly if their surface is loosened. The theory is used to predict the diurnal thermal regimes of saturated and dry sand, loam, and peat soils. |
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