標題: Titlebook: Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience; Volume 2: Hydrologic Ming-ko Woo Book 2008 Springer-Verlag [打印本頁] 作者: 淹沒 時間: 2025-3-21 17:50
書目名稱Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience影響因子(影響力)
書目名稱Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience影響因子(影響力)學科排名
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書目名稱Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience網絡公開度學科排名
書目名稱Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience被引頻次
書目名稱Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience被引頻次學科排名
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書目名稱Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience年度引用學科排名
書目名稱Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience讀者反饋
書目名稱Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience讀者反饋學科排名
作者: 蹣跚 時間: 2025-3-21 22:24 作者: Excise 時間: 2025-3-22 03:57
Analysis and Application of 1-km Resolution Visible and Infrared Satellite Data over the Mackenzie collected at 1-km resolution over the Mackenzie Basin specifically for the Mackenzie GEWEX Study (MAGS) water year and the Canadian GEWEX Enhanced Study period. Through the use of satellite data, clear sky products (land surface temperature, evapotranspiration, water temperature time series over la作者: construct 時間: 2025-3-22 08:03
On the Use of Satellite Passive Microwave Data for Estimating Surface Soil Wetness in the Mackenziesin using SSM/I remotely sensed brightness temperature measurements. The approach accounts for the seasonal evolution of the vegetation state and the basin surface heterogeneity. Results demonstrate that the approach can filter out the vegetation effect and produce reasonable estimates of . at the b作者: crescendo 時間: 2025-3-22 09:09
Studies on Snow Redistribution by Wind and Forest, Snow-covered Area Depletion, and Frozen Soil Infwing snow, interception and sublimation of snow in forest canopies, snow spatial distributions in complex environments, snowmelt in open environments and under forest canopies, advection of energy from bare ground to snow, snowcover depletion during melt, and heat and mass transfer during infiltrati作者: violate 時間: 2025-3-22 15:59 作者: violate 時間: 2025-3-22 17:33
Modeling Maximum Active Layer Thaw in Boreal and Tundra Environments using Limited Data,uatic ecosystems, and the integrity of northern infrastructure, including oil and gas pipelines. For most planning and management purposes, the long-term probability distribution of active layer thickness is of primary interest. This study presents a robust method for calculating maximum active laye作者: hegemony 時間: 2025-3-22 21:25
Climate-Lake Interactions,enience they are classified into small, medium and large in terms of surface area. MRB lakes are subjected to a wide range in air temperature from south to north, and to substantial differences in precipitation. The ice-covered period is a function of lake size and location. Small lakes have a longe作者: essential-fats 時間: 2025-3-23 03:35 作者: 漂泊 時間: 2025-3-23 08:01 作者: 丑惡 時間: 2025-3-23 12:40
Interannual Variability of the Thermal Components and Bulk Heat Exchange of Great Slave Lake,longer-term climatic conditions. The lake is dimictic and exhibits spatial and temporal variability in air temperature and wind speed that impacts water surface temperature and lake heat flux. Storm events with high winds were responsible for short-term highly dynamical responses of the lake, with d作者: 無聊點好 時間: 2025-3-23 13:53
Flow Connectivity of a Lake-Stream System in a Semi-arid Precambrian Shield Environment,nection in the lake-stream system, a chain of lakes in northern Canada was studied in 2004. Water balance shows that rapid and substantial runoff from the local basin slopes during the snowmelt period led to a rise of lake levels above their outlet elevations to generate outflow. Continued summer ev作者: 舊病復發(fā) 時間: 2025-3-23 19:28 作者: 可能性 時間: 2025-3-24 00:29 作者: GILD 時間: 2025-3-24 06:19 作者: GRE 時間: 2025-3-24 08:41 作者: 灰心喪氣 時間: 2025-3-24 11:47
Impact of Climate Change on the Peace River Thermal Ice Regime,the ice regime of the Peace River in Alberta. The model employs an Eulerian frame of reference for both the flow hydrodynamics and the ice processes (ice cover formation and deterioration) and uses the characteristic-dissipative-Galerkin finite element method to solve the primary equations. Model ca作者: arthroscopy 時間: 2025-3-24 18:54
Climate Impacts on Ice-jam Floods in a Regulated Northern River,ice-jam flooding in the lower Peace River has resulted in prolonged dry periods and considerable reduction in the area covered by lakes and ponds that provide habitat for aquatic life in the PAD. Using archived hydrometric data and in situ observations, the ice regime of the lower Peace is quantifie作者: 向外才掩飾 時間: 2025-3-24 19:18
Trends in Mackenzie River Basin Streamflows, annual trends were identified using the Mann-Kendall test with an approach that corrects for serial correlation. The global (or field) significance of the results for each watershed was evaluated using a bootstrap resampling technique. The results reveal more trends in some hydrologic variables tha作者: conference 時間: 2025-3-25 00:19
https://doi.org/10.1007/978-3-540-75136-6Atmospheric; Frost; Hydrologic; Infiltration; Precipitation; Scale; Snow; Storm; climate change; digital elev作者: Yourself 時間: 2025-3-25 06:28
978-3-642-09434-7Springer-Verlag Berlin Heidelberg 2008作者: 分貝 時間: 2025-3-25 09:46
Ming-ko WooUtilizes an integrative approach across disciplines in addressing major research issues of the cold regions.Research presented is applicable to other higher latitude regions in America, Europe and Asi作者: 外面 時間: 2025-3-25 11:46
http://image.papertrans.cn/c/image/229289.jpg作者: 硬化 時間: 2025-3-25 19:34
https://doi.org/10.1007/978-90-481-2503-6nts; their distance from large urban centers raises the cost of logistics and reduces the availability of measured data. Yet, these regions are sensitive to climate variability and change and are prone to accelerated human activities. Improved understanding of the physical processes and enhanced cap作者: 諄諄教誨 時間: 2025-3-25 22:31
https://doi.org/10.1007/978-90-481-2503-6These include the accumulation, sublimation and ablation aspects of the snow in boreal forest and tundra areas; infiltration into and thawing of frozen soil; breakup of river ice and the associated floods. Additionally, there are several land surface features distinctive to the Mackenzie River Basin作者: VOC 時間: 2025-3-26 02:44 作者: crumble 時間: 2025-3-26 07:19
Minhua Ma,Bobbie Fletcher,Tim Marshsin using SSM/I remotely sensed brightness temperature measurements. The approach accounts for the seasonal evolution of the vegetation state and the basin surface heterogeneity. Results demonstrate that the approach can filter out the vegetation effect and produce reasonable estimates of . at the b作者: PAN 時間: 2025-3-26 11:05 作者: 開玩笑 時間: 2025-3-26 13:16 作者: 花費 時間: 2025-3-26 17:02 作者: allude 時間: 2025-3-27 00:58 作者: 灰心喪氣 時間: 2025-3-27 05:01
Tim Marsh,Ashima Thomas,Eng Tat Khoocoefficients (C . ) for each lake and for groups of lakes. Transfer coefficients determined from multiple years of data for the two smallest lakes were similar (1.26 x 10 . and 1.30 x 10 . ) while that for the largest lake was slightly smaller (1.10 x 10 . ). The coefficient for the medium-size lake作者: Picks-Disease 時間: 2025-3-27 09:04
Myfanwy King,Tim Marsh,Zeynep Akcay of time scales on the magnitude and control of the process. Based on measurements using the eddy covariance method, both the latent and sensible heat fluxes were consistently small following ice break up, but increased dramatically as ice formation commenced. Half of the total evaporative water los作者: 泥瓦匠 時間: 2025-3-27 12:51 作者: 美麗的寫 時間: 2025-3-27 15:20
Myfanwy King,Tim Marsh,Zeynep Akcaynection in the lake-stream system, a chain of lakes in northern Canada was studied in 2004. Water balance shows that rapid and substantial runoff from the local basin slopes during the snowmelt period led to a rise of lake levels above their outlet elevations to generate outflow. Continued summer ev作者: Generic-Drug 時間: 2025-3-27 18:22
https://doi.org/10.1007/978-3-030-88272-3e. The northwestern portion of the Shield has a relatively dry, subarctic climate and a heterogeneous landscape comprising exposed bedrock uplands, soil mantled slopes, wetlands and lakes. The water budget of bedrock uplands is influenced by rock fractures, slope aspect, precipitation or melt intens作者: 深陷 時間: 2025-3-28 01:16 作者: Overstate 時間: 2025-3-28 02:06 作者: 沉思的魚 時間: 2025-3-28 09:06
Menna Elshahawy,Said Mostafa,Nada Sharafed damages. However, our ability to forecast such events remains quite limited. An example of this is the Athabasca River at Fort McMurray, Alberta, where severe ice jam events have been documented for over 100 years, and where breakup has been monitored intensively for the past 25 years. Despite th作者: GRILL 時間: 2025-3-28 11:03
Sundus Fatima,Jannicke Baalsrud Haugethe ice regime of the Peace River in Alberta. The model employs an Eulerian frame of reference for both the flow hydrodynamics and the ice processes (ice cover formation and deterioration) and uses the characteristic-dissipative-Galerkin finite element method to solve the primary equations. Model ca作者: 自戀 時間: 2025-3-28 17:11
Menna Elshahawy,Said Mostafa,Nada Sharafice-jam flooding in the lower Peace River has resulted in prolonged dry periods and considerable reduction in the area covered by lakes and ponds that provide habitat for aquatic life in the PAD. Using archived hydrometric data and in situ observations, the ice regime of the lower Peace is quantifie作者: Commission 時間: 2025-3-28 20:21
Menna Elshahawy,Said Mostafa,Nada Sharaf annual trends were identified using the Mann-Kendall test with an approach that corrects for serial correlation. The global (or field) significance of the results for each watershed was evaluated using a bootstrap resampling technique. The results reveal more trends in some hydrologic variables tha作者: 妨礙 時間: 2025-3-28 23:50 作者: 能得到 時間: 2025-3-29 04:22
Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience978-3-540-75136-6作者: 哀悼 時間: 2025-3-29 08:48
from the GEWEX project, dealing with the region‘s atmospheric dynamics. Together these books provide a unique synthesis of atmospheric and hydrological findings and an integrative approach across disciplines in addressing major research issues of cold regions..978-3-642-09434-7978-3-540-75136-6作者: 微塵 時間: 2025-3-29 14:18
On the Use of Satellite Passive Microwave Data for Estimating Surface Soil Wetness in the Mackenzieomponent in estimating the ., and to downscale the index at the digital elevation models scale using a topographic index (.) which is continuously adjusted to account for vegetation growth. When applied to the Peace-Athabasca-Delta area, this method improved the correlation between soil wetness and 作者: 抱怨 時間: 2025-3-29 16:38 作者: 圖畫文字 時間: 2025-3-29 19:54 作者: 高談闊論 時間: 2025-3-30 00:22 作者: hair-bulb 時間: 2025-3-30 04:29 作者: 揭穿真相 時間: 2025-3-30 08:37 作者: 口味 時間: 2025-3-30 13:41
Flow Connectivity of a Lake-Stream System in a Semi-arid Precambrian Shield Environment,nd spill of lakes should be considered in modeling Shield hydrology under semi-arid conditions, to take account of (1) antecedent storage in individual lakes, (2) their storage change calculated through water balance, and (3) the thresholds to be exceeded for outflows to occur.作者: etidronate 時間: 2025-3-30 18:18
Hydrology of the Northwestern Subarctic Canadian Shield,rated in headwaters can be transferred to basin outlets. The subarctic Shield environment has large spatial and temporal variations in available storage, where the hydrologic connectivity that dictates runoff response is controlled in part by the geometry and spatial distribution of landscape compon作者: Exaggerate 時間: 2025-3-30 23:43
Climate Impacts on Ice-jam Floods in a Regulated Northern River,vers would be slightly thinner than they are at present. More importantly, a large part of the Peace River basin is expected to experience frequent and sustained mid-winter thaws. These events are expected to cause significant melt and depleted snowpack in the spring, leading to severe reduction in 作者: 羞辱 時間: 2025-3-31 03:07
Minhua Ma,Bobbie Fletcher,Tim Marshomponent in estimating the ., and to downscale the index at the digital elevation models scale using a topographic index (.) which is continuously adjusted to account for vegetation growth. When applied to the Peace-Athabasca-Delta area, this method improved the correlation between soil wetness and 作者: 講個故事逗他 時間: 2025-3-31 07:12 作者: 辯論 時間: 2025-3-31 11:41 作者: 陳舊 時間: 2025-3-31 14:44
Tim Marsh,Ashima Thomas,Eng Tat Khoogest that the multi-year coefficients give acceptable results for small and medium-size lakes only, and that these coefficients cannot be transferred from one lake to another, unless the lakes are similar in size.作者: NOMAD 時間: 2025-3-31 18:20
Myfanwy King,Tim Marsh,Zeynep Akcayous sampling intervals. Varying the sampling interval from one to six hours in 1-hr steps had no significant effect on the coefficients used to predict the 24-hr evaporation totals. The dichotomy between lake and land surfaces in terms of temporal changes in heat source and sink, and the longer dura作者: 躺下殘殺 時間: 2025-3-31 21:43
Lecture Notes in Computer Scienceure differences. Variation of the 8 ° C isotherm effectively demonstrated interannual variability in the lake heating. Annual heat content ranged from 2.61 × 10. J in 1998 to 2.13 × 10. J in 2002. Five-year mean heat content maximum was 2.24 × 10. J. The bulk heat exchange, ranging between 267 W m. 作者: adipose-tissue 時間: 2025-4-1 02:59
Myfanwy King,Tim Marsh,Zeynep Akcaynd spill of lakes should be considered in modeling Shield hydrology under semi-arid conditions, to take account of (1) antecedent storage in individual lakes, (2) their storage change calculated through water balance, and (3) the thresholds to be exceeded for outflows to occur.作者: 詞匯記憶方法 時間: 2025-4-1 07:11
https://doi.org/10.1007/978-3-030-88272-3rated in headwaters can be transferred to basin outlets. The subarctic Shield environment has large spatial and temporal variations in available storage, where the hydrologic connectivity that dictates runoff response is controlled in part by the geometry and spatial distribution of landscape compon作者: 人類 時間: 2025-4-1 12:49
Menna Elshahawy,Said Mostafa,Nada Sharafvers would be slightly thinner than they are at present. More importantly, a large part of the Peace River basin is expected to experience frequent and sustained mid-winter thaws. These events are expected to cause significant melt and depleted snowpack in the spring, leading to severe reduction in 作者: 沐浴 時間: 2025-4-1 15:59 作者: diathermy 時間: 2025-4-1 19:20 作者: Euthyroid 時間: 2025-4-1 23:21
Lecture Notes in Computer Sciencetrating an enhanced capability to model melt related runoff. Future research is required to accurately model both snow-covered area and runoff at a variety of scales and to incorporate topographic and vegetation effects correctly in the models.作者: Longitude 時間: 2025-4-2 05:51 作者: 相符 時間: 2025-4-2 09:17
