標(biāo)題: Titlebook: Arctic Hydrology, Permafrost and Ecosystems; Daqing Yang,Douglas L. Kane Book 2021 Springer Nature Switzerland AG 2021 Arctic Hydrology.Ar [打印本頁] 作者: 夾子 時間: 2025-3-21 19:55
書目名稱Arctic Hydrology, Permafrost and Ecosystems影響因子(影響力)
書目名稱Arctic Hydrology, Permafrost and Ecosystems影響因子(影響力)學(xué)科排名
書目名稱Arctic Hydrology, Permafrost and Ecosystems網(wǎng)絡(luò)公開度
書目名稱Arctic Hydrology, Permafrost and Ecosystems網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Arctic Hydrology, Permafrost and Ecosystems被引頻次
書目名稱Arctic Hydrology, Permafrost and Ecosystems被引頻次學(xué)科排名
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書目名稱Arctic Hydrology, Permafrost and Ecosystems年度引用學(xué)科排名
書目名稱Arctic Hydrology, Permafrost and Ecosystems讀者反饋
書目名稱Arctic Hydrology, Permafrost and Ecosystems讀者反饋學(xué)科排名
作者: 誘導(dǎo) 時間: 2025-3-21 21:26
Richard Levy,Patricia S. Goldman-Rakice hydrologic gradient makes flow in upward or downward directions. The heat balance of the super-, inter-, or sub- permafrost generates unique unfrozen geometry in the permafrost. This chapter also reviews various cellars developed and used in the arctic regions by indigenous people.作者: Fluctuate 時間: 2025-3-22 02:30
Permafrost Features and Talik Geometry in Hydrologic Systeme hydrologic gradient makes flow in upward or downward directions. The heat balance of the super-, inter-, or sub- permafrost generates unique unfrozen geometry in the permafrost. This chapter also reviews various cellars developed and used in the arctic regions by indigenous people.作者: addition 時間: 2025-3-22 06:49 作者: 新字 時間: 2025-3-22 12:43 作者: slow-wave-sleep 時間: 2025-3-22 13:41 作者: 隱語 時間: 2025-3-22 20:26 作者: 走調(diào) 時間: 2025-3-22 21:36
River Ice Processes and Changes Across the Northern Regionsodeling and remote sensing tools are very useful to the understanding of ice processes, attributions of past changes, and projection of future ice conditions in a warming Arctic. More effort is necessary to combine observations, models, and remote sensing technology to investigate ice hydrology over the broader northern regions.作者: 廚房里面 時間: 2025-3-23 03:17 作者: fiscal 時間: 2025-3-23 08:04
t, and ecosystem.Offers a valuable resource for environmenta.This book provides a comprehensive, up-to-date assessment of the key terrestrial components of the Arctic system, i.e., its hydrology, permafrost, and ecology, drawing on the latest research results from across the circumpolar regions. The作者: INTER 時間: 2025-3-23 13:14 作者: headlong 時間: 2025-3-23 15:30
Regional and Basin Streamflow Regimes and Changes: Climate Impact and Human Effectnd the results of watershed hydrology analyses, including climate impact and influence of human activities, particularly dam regulation. This chapter is closely linked with other chapters of basin snow cover hydrology, and freshwater and heat fluxes into the Arctic Ocean.作者: Inelasticity 時間: 2025-3-23 20:36
Towards a semantics for concurrent ,, Arctic temperature and sea ice. There is evidence for increased moisture content of the Arctic atmosphere and corresponding impacts on episodes of extreme warmth. The recent variations of Arctic temperature and associated variables fit well with the simulations of Arctic climate by global and regio作者: 蹣跚 時間: 2025-3-23 23:18
Executing Magic in the Modern Erar political region using very diverse perspectives and approaches. Here we draw from many of these and remote sensing to piece together studies that illustrate a broader picture of Arctic precipitation conditions and reveal emerging and/or diverging patterns of change. This chapter will (1) introduc作者: Gustatory 時間: 2025-3-24 06:18
Jens Nachtwei Prof. Dr.,Sebastian Uedelhovenhaw processes due to warming also affect land surface conditions and the ET processes. During 1983–2005, ET increased significantly in the Arctic region with a rate of 3.8?mm decade-1 because of regional warming and vegetation greening. Such an increase in ET may exert significant impacts on the reg作者: 托運 時間: 2025-3-24 09:32 作者: Interstellar 時間: 2025-3-24 11:55 作者: 凝結(jié)劑 時間: 2025-3-24 18:45
Tony Chapman,Bill Best,Paul Van Casterenessary to sustain aquatic ecosystems. The goal of this Chapter is to present an overview of environmental flows for permafrost regions, with a focus on North America where information is most readily available. This goal is achieved via a review of (i) cold regions hydro-ecology, (ii) history and ap作者: amnesia 時間: 2025-3-24 20:39 作者: 攀登 時間: 2025-3-25 03:10
Executive Compensation and Shareholder Valueer monitoring location, since water temperature at this site is strongly influenced by the heat storage of Great Bear Lake. Tests of three models, i.e., linear regression, logical regression (s-shape), and the physically based air2stream model, show that the air2stream model provided the best result作者: Dendritic-Cells 時間: 2025-3-25 05:21
Jennifer Carpenter,David Yermackprocesses in Arctic rivers, with particular focus on the cycling of organic carbon, nitrogen and phosphorus species, and a suite of trace elements. Third, we identify uncertainties and current gaps in our knowledge of biogeochemical processes in Arctic rivers and recommend steps forward to address t作者: Virtues 時間: 2025-3-25 10:02
https://doi.org/10.1007/978-1-4757-5192-5aturation (wetland) or storage capacity (lake). Snow is particularly important, and for Arctic wetlands and lakes, it is the total winter snow accumulation that is of major hydrological consequence. Summer rainfall in most permafrost areas is not high, and often is insufficient to match evaporation 作者: LITHE 時間: 2025-3-25 11:47 作者: appall 時間: 2025-3-25 19:19 作者: Expertise 時間: 2025-3-25 21:56 作者: 光亮 時間: 2025-3-26 03:34 作者: Melanocytes 時間: 2025-3-26 07:51 作者: FORGO 時間: 2025-3-26 08:44
Evaporation Processes and Changes Over the Northern Regionshaw processes due to warming also affect land surface conditions and the ET processes. During 1983–2005, ET increased significantly in the Arctic region with a rate of 3.8?mm decade-1 because of regional warming and vegetation greening. Such an increase in ET may exert significant impacts on the reg作者: Morose 時間: 2025-3-26 15:28 作者: 旅行路線 時間: 2025-3-26 17:27 作者: Orchiectomy 時間: 2025-3-26 21:04 作者: fibula 時間: 2025-3-27 02:42 作者: etiquette 時間: 2025-3-27 05:48
Arctic River Water Temperatures and Thermal Regimeser monitoring location, since water temperature at this site is strongly influenced by the heat storage of Great Bear Lake. Tests of three models, i.e., linear regression, logical regression (s-shape), and the physically based air2stream model, show that the air2stream model provided the best result作者: 致敬 時間: 2025-3-27 10:18
Changing Biogeochemical Cycles of Organic Carbon, Nitrogen, Phosphorus, and Trace Elements in Arcticprocesses in Arctic rivers, with particular focus on the cycling of organic carbon, nitrogen and phosphorus species, and a suite of trace elements. Third, we identify uncertainties and current gaps in our knowledge of biogeochemical processes in Arctic rivers and recommend steps forward to address t作者: 小故事 時間: 2025-3-27 14:40 作者: 飛行員 時間: 2025-3-27 18:58
Ground Temperature and Active Layer Regimes and Changes and InSAR application in the northern regions. It is important to emphasize that northern permafrost conditions have significantly changed and will continue to change in the future. In order to understand the past history and future of permafrost, we need to continue and expand the monitoring of th作者: SENT 時間: 2025-3-27 22:30
Towards a semantics for concurrent ,,f the cryosphere, show signals consistent with the warming of the past half century. This Arctic amplification of the warming arises from a number of processes in the climate system, including the feedbacks associated with the loss of sea ice and snow, the increase of atmospheric moisture, and the v作者: Jargon 時間: 2025-3-28 02:41 作者: 把…比做 時間: 2025-3-28 09:09
The Places and Tools of Execution,arge-scale snow cover extent and snow water equivalent (SWE), then moves to the local scale for a discussion of the processes and interactions responsible for the spatial distribution and physical properties of Arctic snow cover, most notably the roles of blowing snow and vegetation interactions. Sn作者: 單片眼鏡 時間: 2025-3-28 13:04
Jens Nachtwei Prof. Dr.,Sebastian Uedelhovener northern regions and watersheds. ET in northern regions tends to increase with the decrease of latitude. The largest ET typically appears in the forest ecosystem, while the grasslands and shrublands have small ET. While the seasonal variations in ET are usually high, the interannual variability i作者: 怎樣才咆哮 時間: 2025-3-28 14:49 作者: surmount 時間: 2025-3-28 21:46
DDI: nachhaltige Assessments in der Praxisct, basin hydrology changed very significant over the past decades. This chapter reviews the research progress of regional flow regimes and changes, and the results of watershed hydrology analyses, including climate impact and influence of human activities, particularly dam regulation. This chapter 作者: 概觀 時間: 2025-3-29 00:32 作者: Pepsin 時間: 2025-3-29 05:44 作者: 咯咯笑 時間: 2025-3-29 07:49 作者: conception 時間: 2025-3-29 15:19 作者: bile648 時間: 2025-3-29 15:45
Jennifer Carpenter,David Yermackadwater streams to larger rivers, estuaries, and the Arctic Ocean. Recent climate change in the Arctic has altered stream and river discharge, temperature, and biogeochemical processes. In this chapter, we summarize the state of research linking watershed hydrology and biogeochemical cycling in Arct作者: embolus 時間: 2025-3-29 20:31
https://doi.org/10.1007/978-1-4757-5192-5uence on the hydrological cycle as they can both store and release water to streams, other wetlands (ponds) and replenish groundwater reserves. Arctic landscapes are also rich with lakes and their occurrence depends on geology, geomorphic or anthropogenic setting. Like ponds, lake sustainability ove作者: 骯臟 時間: 2025-3-30 03:09 作者: 畢業(yè)典禮 時間: 2025-3-30 04:10 作者: 箴言 時間: 2025-3-30 11:32 作者: 調(diào)色板 時間: 2025-3-30 15:33
Victor Tang,Kevin Otto,Warren Seeringh permafrost has a very low hydraulic conductivity and commonly acts as a barrier to deeper groundwater recharge or as a confining layer to deeper aquifers. In regions underlain by permafrost, the active layer is the upper layer of the soil near the surface that undergoes thawing in the summer and f作者: 血友病 時間: 2025-3-30 18:05 作者: NEEDY 時間: 2025-3-31 00:41 作者: 氣候 時間: 2025-3-31 04:37
Daqing Yang,Douglas L. KaneProvides an up-to-date assessment of the key terrestrial components of the Arctic system.Covers linkages between Arctic hydrology, permafrost, and ecosystem.Offers a valuable resource for environmenta作者: 過去分詞 時間: 2025-3-31 08:12 作者: chemical-peel 時間: 2025-3-31 09:26 作者: Adenoma 時間: 2025-3-31 14:01 作者: 人工制品 時間: 2025-3-31 20:51
Snow Cover—Observations, Processes, Changes, and Impacts on Northern Hydrologyarge-scale snow cover extent and snow water equivalent (SWE), then moves to the local scale for a discussion of the processes and interactions responsible for the spatial distribution and physical properties of Arctic snow cover, most notably the roles of blowing snow and vegetation interactions. Sn作者: interlude 時間: 2025-4-1 00:25
Evaporation Processes and Changes Over the Northern Regionser northern regions and watersheds. ET in northern regions tends to increase with the decrease of latitude. The largest ET typically appears in the forest ecosystem, while the grasslands and shrublands have small ET. While the seasonal variations in ET are usually high, the interannual variability i
