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91.
Mikołaj Piniewski Frank Voss Ilona Bärlund Tomasz Okruszko Zbigniew W. Kundzewicz 《水文科学杂志》2013,58(4):737-754
Abstract The effect of using two distributed hydrological models with different degrees of spatial aggregation on the assessment of climate change impact on river runoff was investigated. Analyses were conducted in the Narew River basin situated in northeast Poland using a global hydrological model (WaterGAP) and a catchment-scale hydrological model (SWAT). Climate change was represented in both models by projected changes in monthly temperature and precipitation between the period 2040–2069 and the baseline period, resulting from two general circulation models: IPSL-CM4 and MIROC3.2, both coupled with the SRES A2 emissions scenario. The degree of consistency between the global and the catchment model was very high for mean annual runoff, and medium for indicators of high and low runoff. It was observed that SWAT generally suggests changes of larger magnitude than WaterGAP for both climate models, but SWAT and WaterGAP were consistent as regards the direction of change in monthly runoff. The results indicate that a global model can be used in Central and Eastern European lowlands to identify hot-spots where a catchment-scale model should be applied to evaluate, e.g. the effectiveness of management options. Editor D. Koutsoyiannis; Associate editor F.F. Hattermann Citation Piniewski, M., Voss, F., Bärlund, I., Okruszko, T., and Kundzewicz. Z.W., 2013. Effect of modelling scale on the assessment of climate change impact on river runoff. Hydrological Sciences Journal, 58 (4), 737–754. 相似文献
92.
93.
Hindcasting global temperature by evolutionary computation 总被引:2,自引:1,他引:1
Interpretation of changes of global temperature is important for our understanding of the climate system and for our confidence in projections for the future. Massive efforts have been devoted to improve the accuracy of reproducing the global temperature by the available climate models, but the hindcasts are still inaccurate. Notwithstanding the need to further advance climate models, one may consider data-driven approaches, providing practically useful results in a simpler and faster way. Without assuming any prior knowledge about physics and without imposing a model structure that encapsulates the existing knowledge about the underlying processes, we hindcast global temperature by automatically identified evolutionary computation models. We use 60 years of records of global temperature and climate drivers, with training and testing periods being 1950–1999 and 2000–2009, respectively. This paper demonstrates that the global temperature observed in the past is mimicked with reasonably good accuracy. Evolutionary computation holds promise for modeling the global climate system, which looks hopelessly complex in classical perspective. 相似文献
94.
Toward very high horizontal resolution NWP over the alps: Influence of increasing model resolution on the flow pattern 总被引:1,自引:0,他引:1
Michał Z. Ziemiański Marcin J. Kurowski Zbigniew P. Piotrowski Bogdan Rosa Oliver Fuhrer 《Acta Geophysica》2011,59(6):1205-1235
The increasing resolution of contemporary regional numerical weather prediction (NWP) models, reaching horizontal grid sizes
of O(1 km), requires robust and reliable dynamical cores, working well beyond the approximation of quasi-horizontal flows. That
stimulates an interest in an application for NWP purposes of dynamical cores based on the anelastic, or — more generally —
sound-proof flow equations, and characterized by appropriate robustness and reliability. The paper presents results from testing
the dynamical core of EULAG, the anelastic research model for multi-scale flows, as a prospective NWP dynamical core. The
model simulates the semi-realistic frictionless and adiabatic flow over realistic steep Alpine topographies, employing horizontal
grid sizes of 2.2, 1.1, and 0.55 km. The paper demonstrates not only the numerical robustness of EULAG, but also studies the
influence of the varying horizontal resolution on the simulated flow. Results show that the increased horizontal resolution
increases orographic drag on the flow. While the general flow pattern remains the same, increased resolution influences the
flow on scales from hundreds of kilometers to meso-gamma scales. The differences are especially apparent in the near-surface
layer of 1.5 to 3 km deep, and in the distribution and amplitudes of the orographically-induced gravity waves. 相似文献
95.
96.
97.
Local Scales of Turbulence in the Stable Boundary Layer 总被引:1,自引:1,他引:0
Zbigniew Sorbjan 《Boundary-Layer Meteorology》2008,127(2):261-271
Local, gradient-based scales, which contain the vertical velocity and temperature variances, as well as the potential temperature
gradient, but do not include fluxes, are tested using data collected during the CASES-99 experiment. The observations show
that the scaling based on the temperature variance produces relatively smaller scatter of empirical points. The resulting
dimensionless statistical moments approach constant values for sufficiently large values of the Richardson number Ri. This allows one to derive predictions for the Monin–Obukhov similarity functions φ
m
and φ
h
, the Prandtl number Pr and the flux Richardson number Rf in weak turbulence regime. 相似文献
98.
Data collected during the SHEBA and CASES-99 field programs are employed to examine the flux–gradient relationship for wind
speed and temperature in the stably stratified boundary layer. The gradient-based and flux-based similarity functions are
assessed in terms of the Richardson number Ri and the stability parameter z/Λ*, z being height and Λ* the local Obukhov length. The resulting functions are expressed in an analytical form, which is essentially unaffected by
self-correlation, when thermal stratification is strong. Turbulence within the stably stratified boundary layer is classified
into four regimes: “nearly-neutral” (0 < z/Λ* < 0.02), “weakly-stable” (0.02 < z/Λ* < 0.6), “very-stable” (0.6 < z/Λ* < 50), and “extremely-stable” (z/Λ* > 50). The flux-based similarity functions for gradients are constant in “nearly-neutral” conditions. In the “very-stable”
regime, the dimensionless gradients are exponential, and proportional to (z/Λ*)3/5. The existence of scaling laws in “extremely-stable” conditions is doubtful. The Prandtl number Pr decreases from 0.9 in nearly-neutral conditions and to about 0.7 in the very-stable regime. The necessary condition for the
presence of steady-state turbulence is Ri < 0.7. 相似文献
99.
A statistical model for spatial inventory data: a case study of N2O emissions in municipalities of southern Norway 总被引:1,自引:0,他引:1
In this paper we apply a linear regression with spatial random effect to model geographically distributed emission inventory data. The study presented is on N2O emission assessments for municipalities of southern Norway and on activities related to emissions (proxy data). Taking advantage of the spatial dimension of the emission process, the method proposed is intended to improve inventory extension beyond its earlier coverage. For this, the proxy data are used. The conditional autoregressive model is used to account for spatial correlation between municipalities. Parameter estimation is based on the maximum likelihood method and the optimal predictor is developed. The results indicate that inclusion of a spatial dependence component lead to improvement in both representation of the observed data set and prediction. 相似文献
100.
SAR干涉图作为相位信息的载体,其质量直接影响对研究区域形变状况的进一步分析,采取有效的滤波算法能抑制干涉图相位噪声,提高干涉测量精度。在获得的干涉相位图中,由于矿区开采而造成的地表沉降会体现出近环状相位条纹的特征。针对这一特点,对传统的基于梯度的滤波算法做出了改进,并结合Goldstein频域滤波和改进的梯度自适应滤波,提出了一种适用于矿区沉降形成的SAR干涉相位模式滤波方法。选取河北峰峰煤矿的PALSAR干涉相位图作为实验数据,对该滤波方法做出了详细的性能评价和对比。结果表明,采用本文提出的综合滤波方法在显著降低实验区SAR干涉图相位噪声的同时,也很好地保持了相位分辨率,使由于矿区沉降而造成的形变相位环的边缘形态更加清晰。 相似文献