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  • 1990-1994  (11)
  • 1985-1989  (13)
  • 1
    Monograph available for loan
    Monograph available for loan
    Boundary layer climates (1987)
    London [England] ; New York : Routledge
    Details Availability
    Call number: PIK N 456-94-0117 ; AWI A7-99-0139 ; MOP 47518 / Mitte ; zu MOP 47518 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XXIV, 435 S. : Abb. ; 23 cm
    Edition: 2. ed.
    ISBN: 0415043190
    Location: A 18 - must be ordered
    Location: AWI Reading room
    Location: MOP - must be ordered
    Location: MOP - must be ordered
    Branch Library: PIK Library
    Branch Library: AWI Library
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Urban climatology and its applications with special regard to tropical areas : proceedings of the Technical Conference organized by the World Meteorological Organization and co-sponsored by the World Health Organization (1986)
    Geneva : WMO
    Associated volumes
    Details Availability
    Call number: PIK N 531-10-0246
    In: WMO
    Type of Medium: Monograph available for loan
    Pages: XXIII, 534 S. : graph. Darst.
    Series Statement: WMO / World Meteorological Organization 652
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    The surface energy budgets of urban areas (1987)
    Boston, Mass. : AMS
    Details Availability
    Call number: MOP S 12801
    Type of Medium: Monograph available for loan
    Pages: 52 S.
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Bibliography of urban climate 1981-1988 (1990)
    Geneva : WMO
    Associated volumes
    Details Availability
    Call number: MOP Per 877(15)
    In: World Climate Applications Programme
    In: WMO TD
    Type of Medium: Monograph available for loan
    Pages: V, 62 S.
    Series Statement: World Climate Applications Programme 15
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 5
    Electronic Resource
    Electronic Resource
    Tests of three urban energy balance models (1988)
    Springer
    Boundary layer meteorology 44 (1988), S. 73-96 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Observations of surface characteristics, meteorological conditions and energy balance components from Vancouver, B.C. are used to test the validity of the output from three one-dimensional surface energy balance models. The results show that whereas all of the models provide good simulations of net radiation, none can consistently predict the turbulent fluxes of sensible and latent heat using easily available input data. Inability to handle the role of water availability and its impact on evapotranspiration is identified as the principal problem.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00117293
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  • 6
    Electronic Resource
    Electronic Resource
    Velocity and temperature spectra and cospectra in an unstable suburban atmosphere (1989)
    Springer
    Boundary layer meteorology 47 (1989), S. 309-320 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Boundary-layer flow over very rough surfaces is poorly understood so the applicability of standard micrometeorological theory is uncertain. This study presents observations of the turbulent fluctuations of meteorological parameters over a suburban area. Even though the height of measurement is considered to be close to the junction between the inertial and roughness sub-layers, the wind and temperature spectra and the momentum and sensible heat flux cospectra are in good agreement with reference data from smoother surfaces. Recommendations are made concerning site requirements, height of measurement and averaging times for the study of turbulence and turbulent fluxes over suburban terrain.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00122336
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  • 7
    Electronic Resource
    Electronic Resource
    Urban heat storage derived as energy balance residuals (1987)
    Springer
    Boundary layer meteorology 39 (1987), S. 233-245 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The hourly heat storage changes of a suburban area in Vancouver B.C. are evaluated by residual after determining all other terms in the surface energy balance. Despite the errors and uncertainties associated with this approach, the resulting diurnal cycle of heat storage uptake and release appears to behave in a fashion similar to that of less complex systems. When plotted against the net all-wave radiation, the heat storage values display a hysteresis loop with the peak storage preceding that of radiation. Therefore, although a linear parameterization of heat storage is shown to produce reasonable first-order estimates of storage, a form which includes the time derivative of the net radiation is probably better.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00116120
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  • 8
    Electronic Resource
    Electronic Resource
    Simulation of surface urban heat islands under ‘ideal’ conditions at night part 2: Diagnosis of causation (1991)
    Springer
    Boundary layer meteorology 56 (1991), S. 339-358 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A simple energy balance model which simulates the thermal regime of urban and rural surfaces under calm, cloudless conditions at night is used to assess the relative importance of the commonly stated causes of urban heat islands. Results show that the effects of street canyon geometry on radiation and of thermal properties on heat storage release, are the primary and almost equal causes on most occasions. In very cold conditions, space heating of buildings can become a dominant cause but this depends on wall insulation. The effects of the urban ‘greenhouse’ and surface emissivity are relatively minor. The model confirms the importance of local control especially the relation between street geometry and the heat island and highlights the importance of rural thermal properties and their ability to produce seasonal variation in the heat island. A possible explanation for the small heat
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00119211
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  • 9
    Electronic Resource
    Electronic Resource
    Mixed-layer heat advection and entrainment during the sea breeze (1994)
    Springer
    Boundary layer meteorology 68 (1994), S. 139-158 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A model is developed to simulate the potential temperature and the height of the mixed layer under advection conditions. It includes analytic expressions for the effects of mixed-layer conditions upwind of the interface between two different surfaces on the development of the mixed layer downwind from the interface. Model performance is evaluated against tethersonde data obtained on two summer days during sea breeze flow in Vancouver, Canada. It is found that the mixed-layer height and temperature over the ocean has a small but noticeable effect on the development of the mixed layer observed 10 km inland from the coast. For these two clear days, the subsidence velocity at the inversion base capping the mixed layer is estimated to be about 30 mm s−1 from late morning to late afternoon. When the effects of subsidence are included in the model, the mixed-layer height is considerably underpredicted, while the prediction for the mean potential temperature in the mixed layer is considerably improved. Good predictions for both height and temperature can be obtained when values for the heat entrainment ratio,c, 0.44 and 0.68 for these two days respectively for the period from 1000 to 1300 LAT, were used. These values are estimated using an equation including the additional effects on heat entrainment due to the mechanical mixing caused by wind shear at the top of the mixed layer and surface friction. The contribution of wind shear to entrainment was equal to, or greater than, that from buoyant convection resulting from the surface heat flux. Strong wind shear occurred near the top of the mixed layer between the lower level inland flow and the return flow aloft in the sea breeze circulation.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00712668
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  • 10
    Electronic Resource
    Electronic Resource
    Suburban-rural energy balance comparisons in summer for Vancouver, B.C. (1986)
    Springer
    Boundary layer meteorology 36 (1986), S. 351-369 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Simultaneous energy balance observations at a rural and a suburban site in Vancouver, B.C. during the summer of 1983 are presented. The study is a follow-up to that conducted in 1980. Many of the 1980 results were unexpected and the present study seeks to assess their representativeness. The net radiant, turbulent sensible, and rural soil heat flux densities were measured directly. The suburban heat storage was parameterized and the turbulent latent heat flux densities were resolved as residuals in the energy balances. The 1983 average diurnal energy partitioning for both sites was typical of those quoted in the literature, suggesting that the 1980 results represent an extreme case. Suburban-rural differences showed the suburban area to have a 4% increase in net radiation, a 51% increase in turbulent sensible heat, and a 46% decrease in turbulent latent heat flux density. The values of the average daytime Bowen ratio were 0.46 and 1.28 for the rural and suburban areas, respectively. The sensible heat flux density exhibited relatively large values in the late afternoon and remained directed upward on many summer evenings. Large day-to-day variability in the relative magnitude of the suburban turbulent fluxes may have been due to synoptic influences. In this environment, the turbulent surface and mixed layers are closely coupled because of the low aerodynamic resistance over the rough surface.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00118337
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