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911.
Forest litter exerts an impact on the energy budget of snow surfaces, which lie beneath forest canopies. In this study, we measured shortwave and longwave radiation levels, as well as quantities of Asian spruce (Picea schrenkinan ) forest litter, over 3 snow study plots that representing an open environment, 20% forest canopy openness (20% FCO), and 80% forest canopy openness (80% FCO). The fractional litter coverage (lc ) was obtained through the binarization of digital photographs of forest litter. The effects of forest litter on snow surface albedo (α ), snow surface temperature (T s ), upward shortwave and longwave radiation (K ↑ and L ↑), and sensible heat flux (H ) were then analyzed. According to our results, the energy budget over snow surface influenced by forest litter principally due to forest litter forcing α decrease and T s increase. The effects of forest litter on the energy budget increased with time and lc . We found that forest litter exerted the most significant impact on K ↑ and L ↑ at daytime during the latter stages of the snowmelt period. The influence of forest litter on H was more apparent on windy days. The presence of forest litter increased gains in shortwave radiation and losses in longwave radiation and decreased gains in H . Compared to the simulated energy (K ↑ + L ↑ + H ) over a snow surface without litter, the calculated energy decreased by ?13.4 W/m2 and increased by 9.0 W/m2, respectively, at the 20% FCO and 80% FCO sites during the latter stages of the snowmelt period. Overall, forest litter facilitated snow surface energy gains at the 80% FCO site and impeded them at the 20% FCO site during the latter stages of the snowmelt period. 相似文献
912.
曲堂栋 《中国海洋湖沼学报》1996,(1)
The general features of the seasonal suuface heat budget in the tropical western Pacific Ocean,20°S-20°N, western boundary-160°E, were documented by Qu (1995) using a high-resolution generalcirculation model (GCM, Semtner & Chervin,1992) ard existing observations.Close inspection of thesmaller areas, with the whole region further partitioned into six parts, showed different mechanisms balancethe seasonal surface heat budget in different parts of the region The results of study on five subregionsare detailed in this article. In the equatorial (3°S - 3°N) aed North Equatorial Countercurrent(3°N-9°N) region, the surface the flux the does not change significantly throughout the year, so the surface heat content is determined largely by vertical motion near the equator and roughly helf due to horizontal and halfdue to vertical circulation in the region of the North Equatorial Countercurrent(NECC). In the othersubregions (9°N-20°N, 20°S -11°S aed 11°S -3°S ), however, in addition to ocean dynamics 相似文献
913.
Qu Tang-dong 《中国海洋湖沼学报》1996,14(1):83-90
The general features of the seasonal surface heat budget in the tropical western Pacific Ocean, 20° S–20°N, western boundary
−160°E, were documented by Qu (1995) using a high-resolution general circulation model (GCM, Semtner & Chervin, 1992) and
existing observations. Close inspection of the smaller areas, with the whole region further partitioned into six parts, showed
different mechanisms balance the seasonal surface heat budget in different parts of the region. The results of study on five
subregions are detailed in this article. In the equatorial (3°S–3°N) and North Equatorial Countercurrent (3°N–9°N) region,
the surface heat flux does not change significantly throughout the year, so the surface heat content is determined largely
by vertical motion near the equator and roughly half due to horizontal and half due to vertical circulation in the region
of the North Equatorial Countercurrent (NECC). In the other subrigions (9°N–20°N, 20°S–11°S and 11°S–3°S), however, in addition
to ocean dynamics, surface heat flux can also play a major role in the seasonal variation of sea surface temperature (SST).
The remotely forced baroclinic waves and their effect on the surface heat storage in the model are also investigated. Comparison
with observations indicates that the model wave activities are reasonably realistic.
Contribution No. 2396 from the Institute of Oceanology, Chinese Academy of Sciences.
This study was supported by the Australian CSIRO Division of Oceanography and the National Natural Science Foundation of China
(No. 49176255) 相似文献
914.
915.
A 1-D model of the formation and seasonal evolution of Polar Stratospheric Clouds (PSCs) is described. The model considers PSCs of types 1 and 2 in the vertical range from 8 to 30 km and utilizes real temperature data. The micro-physical processes included in the model are the heterogeneous nucleation and condensation (or evaporation), while sedimentation, gas diffusion and vertical wind velocity are the processes responsible for transport. Model simulations have been compared with PSC data obtained by lidar at the South Pole: results for the winter 1990 are discussed. The different contribution of type 1 and type 2 PSCs to the measured backscattering coefficient has been evidenced. In the simulations, layers of NAT particles form when low values of the backscattering coefficient are measured; similarly, ice particles form when sharper and rapidly changeable structures with higher values of the backscattering coefficient are observed. Significant results on the condensation and depletion of HNO3 and H2O are presented. Water vapor profiles measured during winter 1990 are reproduced quite well. 相似文献
916.
. The excess radio-path delay due to the atmospheric water vapor, the wet delay, can be derived from water vapor radiometer
(WVR) measurements. WVR data used for external calibration of space geodetic measurements are not always acquired in the directions
of the space geodetic signal sources, thus extrapolation and interpolation methods for the wet delay are needed. We evaluate
three different methods using approximately 10 days of WVR measurements. Two methods, the gradient method and turbulence method,
use the directional information in the data, while the third method used is linear regression in time regardless of the direction
of the observations. The turbulence method yielded at least 10% less RMS estimation error than the errors from the other two
methods.
Received: 20 May 1997 / Accepted: 15 December 1997 相似文献
917.
THE APPROACH TO REMOTE SENSING OF WATER VAPOR BASED ON GPS AND LINEAR REGRESSION Tm IN EASTERN REGION OF CHINA
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The approach to remote sensing of water vapor by using global positioning systems(GPS) isdiscussed.In order to retrieve the vertical integrated water vapor(IWV) or the precipitable water(PW),the weighted "mean temperature" of the atmosphere,Tm would be estimated to the specificarea and season.Tm depends on surface temperature,tropospheric temperature profile,and thevertical distribution of water vapor.The surface temperature dependence is borne out by acomparison of Tm and the values of surface temperature Ts using radiosonde profiles of BeijingStation(No.54511) throughout 1992.The analysis of radiosonde profiles spanning a one-yearinterval(1992) from sites in eastern region of China with a latitude range of 20-50°N and alongitude range of 100-130°E yields the coefficients a and b of a linear regression equation Tm=a+bTs. 相似文献
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