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1.
Michiaki Sugita Tetsuya Hiyama Nobuhiko Endo Shao-Fen Tian 《Boundary-Layer Meteorology》1995,73(1-2):145-158
Careful micrometeorological measurements on an empty parking lot allowed determination of the surface fluxes of sensible heatH and of momentum by applying profile equations derived from Monin-Obukhov similarity theory with two sets of the stability correction function for momentum
m
and sensible heat
h
. These fluxes were compared with reference values ofH independently determined by means of an eddy correlation technique. In general, better agreement was found betweenH values derived from profiles with the stability functions of Brutsaert (1992) and referenceH values, than when the Businger-Dyer functions were used to deriveH. The disagreement in the latter comparison was especially serious under strongly unstable conditions, with the value ofy=–z/L (wherez is the height andL is the Obukhov length) larger than 10. A closer look at the procedure for calculatingH from the profiles revealed that the large differences between theH values derived with these two different versions of the stability correction functions were caused by the small differences of the
h
values, and not by the larger differences of the
m
values. This result stems from the strong sensitivity of the resultingH values on the choice of
h
. 相似文献
2.
Takashi Doi Michiaki Takano Kei Okamura Tamaki Ura Toshitaka Gamo 《Journal of Oceanography》2008,64(3):471-477
We present the results of a chemical survey at a submarine volcano, Teishi Knoll, obtained using a submersible in-situ Mn
analyzer (GAMOS) mounted on an autonomous underwater vehicle (AUV) platform. During this survey, high-resolution data of dissolved
Mn were obtained in three dimensions in nearly real time. The AUV enabled continuous detailed observations along a preprogrammed
pathway, which could not have been performed with conventional CTD hydrocasts. During this observation, anomalously high dissolved
Mn concentrations were obtained within the crater, corresponding to high water temperatures. The anomalies might be a hydrothermal
signature due to volcanic activity from the crater. 相似文献
3.
Frost heaving is a well-known phenomenon in cold regions, which may occur in wet clayey grounds during winter. Railway track upheaval occurring in cold regions during the winter is generally understood as frost heaving in the subgrade layer. However, it has been confirmed that upheaval due to frost heaving sometimes occurs in the ballast layer. This understanding has been observed in active railways in northern Japan. The samples collected from ballast and subgrade layers have been examined for frost heave susceptibilities and confirmed that ballast layers which contain fines may heave. 相似文献
4.
Michiaki Sugita Akihiro Matsuno Rushdi M. M. El-Kilani Ahmed Abdel-Fattah M. A. Mahmoud 《水文科学杂志》2017,62(10):1618-1635
Eddy correlation measurements within the Nile Delta allowed the determination of evapotranspiration (E) for seven crops (rice, maize, cotton, sugar beet, berseem, wheat and fava beans) using basin irrigation (BI), furrow irrigation (FI), BI with increased intervals (BIi), FI with increased intervals (FIi), strip irrigation (SI) and drip irrigation (DI). Total E values over the cropping season for rice (BI, BIi) were the highest (>600 mm), while those for sugar beet (DI), maize (SI and DI) and berseem (BIi) were the lowest (<250 mm). The differences were due to a combination of atmospheric demand, soil moisture, the presence of surface standing water, root depth, and the length and timing of the cropping season. The DI and SI methods had the advantage for water saving, while the FIi and BIi methods were effective for crops with shallow root lengths. Estimated annual E was 566–828 mm/year (water-saving irrigation) and 875–1225 mm/year (conventional irrigation). 相似文献
5.
Profiles of wind velocity and temperature in the outer region of the atmospheric boundary layer (ABL) were used together with surface temperature measurements, to determine regional shear stress and sensible heat flux by means of transfer parameterizations on the basis of bulk similarity. The profiles were measured by means of radiosondes and the surface temperatures by infrared radiation thermometry over hilly prairie terrain in northeastern Kansas during the First ISLSCP Field Experiment (FIFE). In the analysis, the needed similarity functions were determined and tested; the main scaling variables used for the ABL were h
i
, the height of the convectively mixed layer, and V
a
and a, the wind speed and potential temperature averaged over the mixed layer. Good agreement (r = 0.80) was obtained between values of friction velocity u
*
determined by this ABL bulk similarity approach and those obtained by Monin-Obukhov similarity in the surface sublayer. Similarly, values of surface flux of sensible heat H determined by this method compared well (r = 0.90) with the regional means measured at six ground stations. The corresponding regional evaporation values, determined with the energy budget equation, also compared favorably (r = 0.94). 相似文献
6.
A series of experiments carried out in a pasture field during a growing season, allowed a radiometric determination of the scalar roughness for sensible heatz
oh,r
. The values ofz
oh,r
are shown to vary over the range of 10–1–10–7m both diurnally and seasonally, and an existing theoretical model for the estimation of scalar roughness for sensible heat is found to be inappropriate for the precise estimation ofz
oh,r
. To parameterizez
oh,r
better, a multiple regression analysis was performed, with predictor candidates such as solar elevation, solar radiationR
s
, leaf area index LAI, canopy height, the ratio of the solar radiation and the extraterrestrial radiationR
s
/R
e
, the ratio of the direct and the total solar radiationR
d
/R
s
, and the roughness Reynolds number among others. The best regression equation which usesR
s
, LAI,R
s
/R
e
, andR
d
/R
s
is derived withr=0.75; with smaller numbers of predictors, values ofr tend to deteriorate gradually down tor=0.52 when only one predictor, LAI, was incorporated into the equation. 相似文献
7.
Several formulations and proposals to determine the value of the radiometric scalar roughness for sensible heatz
0h,r
are tested with respect to their performance in the estimation of the sensible heat flux by means of the profile equations derived from Monin-Obukhov similarity theory. The equations are applied to the data set of spatially averaged surface skin temperature and profiles of wind speed and temperature observed in a pasture field during a growing season. The use of a physical model developed for a dense canopy to estimate scalar roughness for sensible heatz
0h,r
produced sensible heat fluxH with a correlation coefficientr=0.884, the ratio of means being H
s
/H=1.19 in a comparison with reference values ofH
s
. In comparison, a proposal for a fixed value ofz
0h
yieldedr=0.887, H
s
/H=0.879. In both cases, the validity ofz
0h
=z
0h,r
was assumed. All expressions derived to estimatez
0h,r
from a multiple linear regression with such predictors as leaf area index, solar radiation and the ratio of solar radiation to extraterrestrial radiation, were found to produce a better result, withr better than 0.90 and H
s
/H around 1.0. However, when the constantsc andf of a linear regression equationHs=cH+f are used to evaluate the equations, a marked difference in performance of each formulation appeared. In general, equations with smaller numbers of predictors tend to produce a biased result, i.e., an overestimation ofH at largeH
s
. These values ofH are used in conjunction with the energy balance equation to derive values of the latent heat fluxLE, which are shown to be in good agreement with the reference valuesLE
s
, withr greater than 0.97. 相似文献
8.
发泡颗粒混合轻量土及其原位力学性质 总被引：4，自引：0，他引：4
发泡颗粒混合轻量土是轻量土中的一种,根据需要,可以通过调整发泡颗粒和土的比例来控制混合土的物理、力学性质。本文介绍了发泡颗粒混合轻量土在高速公路桥梁上的另一应用新技术。为了尽量减小隧道开挖的弃碴对桥墩产生的不利影响,在桥墩周围填筑发泡颗粒混合轻量土,以保持原设计桥梁的结构、强度和变形性能。原位试验结果表明,发泡颗粒混合轻量土易于变形,且可极大地减小土的静止土压力,因而可以减小隧道弃碴对桥墩的影响。它作为缓冲材料的应用是成功的,其效果明显。 相似文献
9.
10.
Michiaki Sugita 《水文科学杂志》2020,65(3):401-414
ABSTRACTThe spatial variability of the lake surface energy balance and its causes are not well-understood. Energy balance maps (90 m resolution) of Lake Kasumigaura (172 km2), Japan, obtained by interpolating station data and bulk equations, allowed an investigation of these issues. Due to lake-scale variations in meteorological variables and small-scale fluctuations of surface temperature, Ts, surface heat fluxes differed horizontally at two distinct scales, while radiative fluxes were more uniform. As the key variable to surface flux Ts was only homogeneous for directions with a longer fetch or under calm wind conditions. Using these findings, the suitability of two flux station locations, one at the centre of the lake and another within a cove, was considered. Although both locations satisfied the fetch requirements, Ts was not always found to be homogeneous in the cove, making this location less suitable for flux measurements, an issue that, to date, has been overlooked. 相似文献