標(biāo)題: Titlebook: Distributed Hydrologic Modeling Using GIS; Baxter E. Vieux Book 20011st edition Springer Science+Business Media B.V. 2001 Infiltration.agr [打印本頁] 作者: dabble 時(shí)間: 2025-3-21 18:39
書目名稱Distributed Hydrologic Modeling Using GIS影響因子(影響力)
書目名稱Distributed Hydrologic Modeling Using GIS影響因子(影響力)學(xué)科排名
書目名稱Distributed Hydrologic Modeling Using GIS網(wǎng)絡(luò)公開度
書目名稱Distributed Hydrologic Modeling Using GIS網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Distributed Hydrologic Modeling Using GIS被引頻次
書目名稱Distributed Hydrologic Modeling Using GIS被引頻次學(xué)科排名
書目名稱Distributed Hydrologic Modeling Using GIS年度引用
書目名稱Distributed Hydrologic Modeling Using GIS年度引用學(xué)科排名
書目名稱Distributed Hydrologic Modeling Using GIS讀者反饋
書目名稱Distributed Hydrologic Modeling Using GIS讀者反饋學(xué)科排名
作者: 租約 時(shí)間: 2025-3-21 20:57 作者: justify 時(shí)間: 2025-3-22 03:31
Surface Generation,eration of raster surfaces from data points. Given the many surface generation utilities available within general purpose GIS packages such as ArcView or GRASS, it is important to understand how these surfaces are generated and some of the pitfalls. Figure 3.1 shows the hillslope shaded image of the作者: 逢迎白雪 時(shí)間: 2025-3-22 04:43
Information Content and Spatial Variability,ufficient to capture spatial information. In the following sections we first examine the background and theory of informational entropy; how this statistic serves as a measure of spatial variability; and an application showing the effects of resolution on slope derived from a raster DEM. Using infor作者: Feckless 時(shí)間: 2025-3-22 11:09
Infiltration,gure 5.1 shows an eroded ski slope in Kalkaskia County, Michigan. The Kalkaskia soil is of glacial origin with permeability in excess of 24 cm/hr. Surface runoff and subsequent erosion was possible only because surface vegetation had been removed for construction and raindrop impact caused surface s作者: misanthrope 時(shí)間: 2025-3-22 15:52 作者: misanthrope 時(shí)間: 2025-3-22 21:05 作者: 茁壯成長(zhǎng) 時(shí)間: 2025-3-23 00:49
Precipitation,igure 8.2. Reflectivity depends on the distribution of raindrop sizes with higher reflectivity (>35 dBZ) shown in black representing more intense rainfall. Radar is an important source of spatially and temporally distributed rainfall data for hydrologic modeling. This chapter deals with the use of w作者: expire 時(shí)間: 2025-3-23 04:32 作者: Ingredient 時(shí)間: 2025-3-23 08:54
Calibration,ion considered, the equation modeled, and the associated data sets. The often-stated advantage of physics-based or deterministic representation of distributed hydrologic processes is that parameters having physical significance are properties of the media. Under this tenant, hydraulic roughness is a作者: 污穢 時(shí)間: 2025-3-23 12:15 作者: Consensus 時(shí)間: 2025-3-23 17:11
Book 20011st editiond at how millions of dollars in contract monies were spent based on simplistic hydrologic models. As project engineer in western Kansas, I was responsible for building flood control dams (authorized under Public Law 566) in the Wet Walnut River watershed. This watershed is within the Arkansas-Red Ri作者: 厭惡 時(shí)間: 2025-3-23 18:50 作者: 厭惡 時(shí)間: 2025-3-24 00:11
Drainage Network and Topography, adjustment at larger cell sizes. This chapter identifies a scaling relationship of the drainage network derived at one resolution to those obtained at larger resolutions. Implicit in the discharge-scaling relationship is the fractal dimension of the drainage network.作者: 與野獸博斗者 時(shí)間: 2025-3-24 02:22 作者: capsaicin 時(shí)間: 2025-3-24 09:32
https://doi.org/10.1057/9780230253049ealing, producing runoff Infiltration rate was reduced because of the sealing effect. Understanding problems such as these is important when modeling runoff from natural or disturbed soils resulting from infiltration excess, which this chapter deals with.作者: 急急忙忙 時(shí)間: 2025-3-24 12:50
Infiltration,ealing, producing runoff Infiltration rate was reduced because of the sealing effect. Understanding problems such as these is important when modeling runoff from natural or disturbed soils resulting from infiltration excess, which this chapter deals with.作者: Pseudoephedrine 時(shí)間: 2025-3-24 14:50 作者: 支柱 時(shí)間: 2025-3-24 19:31
https://doi.org/10.1057/9780230253049tour lines drawn photogrammetrically from stereo-aerial photographs. Algorithms for generating such surface are important in distributed hydrologic modeling. Three surface generation schemes will be examined, followed by an application to a catchment located in the Sahel region of West Africa.作者: 圍巾 時(shí)間: 2025-3-25 03:07
Data Sources and Structures, satellites, and other remote sensing techniques typically average some surrogate measure over a volume or area. This chapter addresses issues of data structure, projection, scale, dimensionality, and sources of data for hydrologic applications.作者: mortuary 時(shí)間: 2025-3-25 04:44 作者: 我不重要 時(shí)間: 2025-3-25 07:29 作者: 抱狗不敢前 時(shí)間: 2025-3-25 13:02
https://doi.org/10.1057/9780230253049ry to use GIS to model hydrologic processes, i.e., the spatial and temporal distribution of the inputs and parameters controlling surface runoff. GIS maps describing topography, land use and cover, soils, rainfall, and meteorological variables may become model parameters or inputs in the simulation of hydrologic processes.作者: 血友病 時(shí)間: 2025-3-25 17:10
https://doi.org/10.1057/9780230270794 adjustment at larger cell sizes. This chapter identifies a scaling relationship of the drainage network derived at one resolution to those obtained at larger resolutions. Implicit in the discharge-scaling relationship is the fractal dimension of the drainage network.作者: GRE 時(shí)間: 2025-3-25 22:42
The British Commonwealth and Empireng from rainfall intensities exceeding the infiltration rate of the soil surface. Figure 9.1 shows the grid cell representation and drainage network used by ., a water quantity model. This chapter presents the mathematical analogy and numerical algorithms used in . to solve the governing equations.作者: Ethics 時(shí)間: 2025-3-26 03:02
https://doi.org/10.1057/9780230253049ial detail necessary for hydrologic modeling. If a larger resolution captures essentially the same information as a smaller resolution, it is preferable because computer storage and computational effort will be more efficient.作者: 有雜色 時(shí)間: 2025-3-26 05:26 作者: 污點(diǎn) 時(shí)間: 2025-3-26 11:39 作者: NAUT 時(shí)間: 2025-3-26 12:39 作者: 不利 時(shí)間: 2025-3-26 18:59
https://doi.org/10.1057/9780230253049eration of raster surfaces from data points. Given the many surface generation utilities available within general purpose GIS packages such as ArcView or GRASS, it is important to understand how these surfaces are generated and some of the pitfalls. Figure 3.1 shows the hillslope shaded image of the作者: Palpitation 時(shí)間: 2025-3-27 00:59 作者: 侵略 時(shí)間: 2025-3-27 03:39
https://doi.org/10.1057/9780230253049gure 5.1 shows an eroded ski slope in Kalkaskia County, Michigan. The Kalkaskia soil is of glacial origin with permeability in excess of 24 cm/hr. Surface runoff and subsequent erosion was possible only because surface vegetation had been removed for construction and raindrop impact caused surface s作者: BLANK 時(shí)間: 2025-3-27 08:36
The British Commonwealth and Empire of the cover such as that found under the tree canopies. A general land use/cover map may show this as agricultural or even as an orchard. However, the correct hydraulic roughness depends on the vegetative cover on the soil surface. Deriving hydraulic roughness coefficients for such land use classi作者: 暖昧關(guān)系 時(shí)間: 2025-3-27 13:13 作者: 鞠躬 時(shí)間: 2025-3-27 16:40 作者: A精確的 時(shí)間: 2025-3-27 18:11
The British Commonwealth and Empire a Geographic Information System (GIS). Digital maps of soils, land use, topography and rainfall rates are used to direct runoff, or . runoff, resulting from rainfall intensities exceeding the infiltration rate of the soil surface. Figure 9.1 shows the grid cell representation and drainage network u作者: 自戀 時(shí)間: 2025-3-27 22:35 作者: 壓碎 時(shí)間: 2025-3-28 05:27
The British Commonwealth and Empire is that the spatial variation of parameters and rainfall input is incorporated into the model response. Each parameter and rainfall input has its own spatial variability, which can be characterized by informational entropy (see Chapter 4). Lumping of the parameter, i.e., taking the mean of a parame作者: innate 時(shí)間: 2025-3-28 09:41 作者: APRON 時(shí)間: 2025-3-28 13:07
The British Commonwealth and Empire of the cover such as that found under the tree canopies. A general land use/cover map may show this as agricultural or even as an orchard. However, the correct hydraulic roughness depends on the vegetative cover on the soil surface. Deriving hydraulic roughness coefficients for such land use classification schemes is the theme of this chapter.作者: Efflorescent 時(shí)間: 2025-3-28 14:35
Hydraulic Roughness, of the cover such as that found under the tree canopies. A general land use/cover map may show this as agricultural or even as an orchard. However, the correct hydraulic roughness depends on the vegetative cover on the soil surface. Deriving hydraulic roughness coefficients for such land use classification schemes is the theme of this chapter.作者: semiskilled 時(shí)間: 2025-3-28 19:31 作者: 讓空氣進(jìn)入 時(shí)間: 2025-3-29 02:43 作者: 殺菌劑 時(shí)間: 2025-3-29 05:40
Springer Science+Business Media B.V. 2001作者: 召集 時(shí)間: 2025-3-29 09:36 作者: 統(tǒng)治人類 時(shí)間: 2025-3-29 12:45 作者: congenial 時(shí)間: 2025-3-29 16:57 作者: finale 時(shí)間: 2025-3-29 23:48
Calibration,olution. In fact, it changes according to the fractal scaling law with dimension 2. Thus, even though the model equations are based on conservation equations of mass and momentum, the parameters are scale-dependent. This dependency arises from changes in drainage length, slope, and parameter values 作者: 相互影響 時(shí)間: 2025-3-30 02:32 作者: 征服 時(shí)間: 2025-3-30 05:23
