Use of Models for Water Resources Management, Planning, and Policy
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Proposed 2021-2022 Ice Fishing Contests
Proposed 2021-2022 Ice Fishing Contests Region Contest Name Dates & Waterbody Species of Fish Contest ALS # Contact Telephone Hours Sponsor Person 1 23rd Annual Teena Feb. 12, Lake Mary Yellow Perch, Treasure State 01/01/1500 Chancy 406-314- Frank Family Derby 2022 6am- Ronan Kokanee Angler Circuit -3139 Jeschke 8024 1pm Salmon 1 50th Annual Jan. 8, 2022 Smith Lake Yellow Perch, Sunriser Lions 01/01/1500 Warren Illi 406-890- Sunriser Lions 7am-1pm Northern Pike, Club of Kalispell -323 0205 Family Fishing Sucker Derby 1 Bull Lake Ice Feb. 19-20, Bull Lake Nothern Pike Halfway House 01/01/1500 Dave Cooper 406-295- Fishing Derby 2022 6am- Bar & Grill -3061 4358 10pm 1 Canyon Kid Feb. 26, Lion Lake Trout, Perch Canyon Kids 01/01/1500 Rhonda 406-261- Christmas Lion 2022 10am- Christmas -326 Tallman 1219 Lake Fishing Derby 2pm 1 Fisher River Valley Jan. 29-30, Upper, Salmon, Yellow Fisher River 01/01/1500 Chelsea Kraft 406-291- Fire Rescue Winter 2022 7am- Middle, Perch, Rainbow Valley Fire -324 2870 Ice Fishing Derby 5pm Lower Trout, Northern Rescue Auxilary Thompson Pike Lakes, Crystal Lake, Loon Lake 1 The Lodge at Feb. 26-27, McGregor Rainbow Trout, The Lodge at 01/01/1500 Brandy Kiefer 406-858- McGregor Lake 2022 6am- Lake Lake Trout McGregor Lake -322 2253 Fishing Derby 4pm 1 Perch Assault #2- Jan. 22, 2022 Smith Lake Yellow Perch, Treasure State 01/01/1500 Chancy 406-314- Smith Lake 8am-2pm Nothern Pike Angler Circuit -3139 Jeschke 8024 1 Perch Assault- Feb. -
Effects of Ice Formation on Hydrology and Water Quality in the Lower Bradley River, Alaska Implications for Salmon Incubation Habitat
ruses science for a changing world Prepared in cooperation with the Alaska Energy Authority u Effects of Ice Formation on Hydrology and Water Quality in the Lower Bradley River, Alaska Implications for Salmon Incubation Habitat Water-Resources Investigations Report 98-4191 U.S. Department of the Interior U.S. Geological Survey Cover photograph: Ice pedestals at Bradley River near Tidewater transect, February 28, 1995. Effects of Ice Formation on Hydrology and Water Quality in the Lower Bradley River, Alaska Implications for Salmon Incubation Habitat by Ronald L. Rickman U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 98-4191 Prepared in cooperation with the ALASKA ENERGY AUTHORITY Anchorage, Alaska 1998 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Thomas J. Casadevall, Acting Director Use of trade names in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey. For additional information: Copies of this report may be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 4230 University Drive, Suite 201 Box 25286 Anchorage, AK 99508-4664 Denver, CO 80225-0286 http://www-water-ak.usgs.gov CONTENTS Abstract ................................................................. 1 Introduction ............................................................... 1 Location of Study Area.................................................. 1 Bradley Lake Hydroelectric Project ....................................... -
Vibrational Spectra of Light and Heavy Water with Application to Neutron Cross Section Calculations J
CORE Metadata, citation and similar papers at core.ac.uk Provided by CONICET Digital Vibrational spectra of light and heavy water with application to neutron cross section calculations J. I. Marquez Damian, D. C. Malaspina, and J. R. Granada Citation: J. Chem. Phys. 139, 024504 (2013); doi: 10.1063/1.4812828 View online: http://dx.doi.org/10.1063/1.4812828 View Table of Contents: http://jcp.aip.org/resource/1/JCPSA6/v139/i2 Published by the AIP Publishing LLC. Additional information on J. Chem. Phys. Journal Homepage: http://jcp.aip.org/ Journal Information: http://jcp.aip.org/about/about_the_journal Top downloads: http://jcp.aip.org/features/most_downloaded Information for Authors: http://jcp.aip.org/authors Downloaded 11 Jul 2013 to 200.0.233.52. This article is copyrighted as indicated in the abstract. Reuse of AIP content is subject to the terms at: http://jcp.aip.org/about/rights_and_permissions THE JOURNAL OF CHEMICAL PHYSICS 139, 024504 (2013) Vibrational spectra of light and heavy water with application to neutron cross section calculations J. I. Marquez Damian,1,a) D. C. Malaspina,2 and J. R. Granada1,b) 1Neutron Physics Department and Instituto Balseiro, Centro Atómico Bariloche, CNEA, Argentina 2Department of Biomedical Engineering and Chemistry of Life Processes Institute, Northwestern University, 2145 Sheridan Road, Evanston, Illinois 60208, USA (Received 4 June 2013; accepted 19 June 2013; published online 11 July 2013) The design of nuclear reactors and neutron moderators require a good representation of the interac- tion of low energy (E < 1 eV) neutrons with hydrogen and deuterium containing materials. These models are based on the dynamics of the material, represented by its vibrational spectrum. -
The Incredible Lightness of Water Vapor
1 The Incredible Lightness of Water Vapor ∗ 2 Da Yang and Seth Seidel 3 University of California, Davis 4 Lawrence Berkeley National Laboratory, Berkeley ∗ 5 Corresponding author address: Da Yang, 253 Hoagland Hall, Davis, CA 95616. 6 E-mail: [email protected] Generated using v4.3.2 of the AMS LATEX template 1 ABSTRACT 7 The molar mass of water vapor is significantly less than that of dry air. This 8 makes a moist parcel lighter than a dry parcel of the same temperature and 9 pressure. This effect is referred to as the vapor buoyancy effect and has of- 10 ten been overlooked in climate studies. We propose that this effect increases 11 Earth’s outgoing longwave radiation (OLR) and stabilizes Earth’s climate. 12 We illustrate this mechanism in an idealized tropical atmosphere, where there 13 is no horizontal buoyancy gradient in the free troposphere. To maintain the 14 uniform buoyancy distribution, temperature increases toward dry atmosphere 15 columns to compensate reduction of vapor buoyancy. The temperature differ- 16 ence between moist and dry columns would increase with climate warming 17 due to increasing atmospheric water vapor, leading to enhanced OLR and 18 thereby stabilizing Earth’s climate. We estimate that this feedback strength 2 19 is about O(0.2 W/m /K), which compares with cloud feedbacks and surface 20 albedo feedbacks in current climate. 2 21 1. Introduction 22 How fast would Earth’s climate respond to increasing CO2 (Manabe and Wetherald 1975; Flato 23 et al. 2013; Collins et al. 2013)? Why is tropical climate more stable than extratropical climate 24 (Holland and Bitz 2003; Polyakov et al. -
“Mining” Water Ice on Mars an Assessment of ISRU Options in Support of Future Human Missions
National Aeronautics and Space Administration “Mining” Water Ice on Mars An Assessment of ISRU Options in Support of Future Human Missions Stephen Hoffman, Alida Andrews, Kevin Watts July 2016 Agenda • Introduction • What kind of water ice are we talking about • Options for accessing the water ice • Drilling Options • “Mining” Options • EMC scenario and requirements • Recommendations and future work Acknowledgement • The authors of this report learned much during the process of researching the technologies and operations associated with drilling into icy deposits and extract water from those deposits. We would like to acknowledge the support and advice provided by the following individuals and their organizations: – Brian Glass, PhD, NASA Ames Research Center – Robert Haehnel, PhD, U.S. Army Corps of Engineers/Cold Regions Research and Engineering Laboratory – Patrick Haggerty, National Science Foundation/Geosciences/Polar Programs – Jennifer Mercer, PhD, National Science Foundation/Geosciences/Polar Programs – Frank Rack, PhD, University of Nebraska-Lincoln – Jason Weale, U.S. Army Corps of Engineers/Cold Regions Research and Engineering Laboratory Mining Water Ice on Mars INTRODUCTION Background • Addendum to M-WIP study, addressing one of the areas not fully covered in this report: accessing and mining water ice if it is present in certain glacier-like forms – The M-WIP report is available at http://mepag.nasa.gov/reports.cfm • The First Landing Site/Exploration Zone Workshop for Human Missions to Mars (October 2015) set the target -
Computational Investigation of Surface Freezing in a Molecular Model Of
Computational investigation of surface freezing in a molecular model of water Amir Haji-Akbari ( )a,1 and Pablo G. Debenedettia,2 aDepartment of Chemical and Biological Engineering, Princeton University, Princeton, NJ 08544 Contributed by Pablo G. Debenedetti, February 17, 2017 (sent for review December 21, 2016; reviewed by Christoph Dellago and Angelos Michaelides) Water freezes in a wide variety of low-temperature environ- is therefore one of the major open challenges of atmospheric ments, from meteors and atmospheric clouds to soil and bio- sciences. logical cells. In nature, ice usually nucleates at or near inter- One major difficulty in constructing such predictive frame- faces, because homogenous nucleation in the bulk can only be works is the inability to determine the proper scaling of observed at deep supercoolings. Although the effect of proximal volumetric nucleation rates with the size of microdroplets and surfaces on freezing has been extensively studied, major gaps in nanodroplets that constitute clouds. This is practically impor- understanding remain regarding freezing near vapor–liquid inter- tant because atmospheric clouds are composed of droplets of faces, with earlier experimental studies being mostly inconclu- different sizes. This scaling is determined by whether freezing is sive. The question of how a vapor–liquid interface affects freez- enhanced or suppressed near vapor–liquid interfaces. If freezing ing in its vicinity is therefore still a major open question in ice is suppressed at a free interface, the effective volumetric nucle- physics. Here, we address this question computationally by using ation rate will be independent of r, the droplet radius, and bulk the forward-flux sampling algorithm to compute the nucleation freezing will be dominant at all sizes. -
Systems Approach to Management of Water Resources—Toward Performance Based Water Resources Engineering
water Article Systems Approach to Management of Water Resources—Toward Performance Based Water Resources Engineering Slobodan P. Simonovic Department of Civil and Environmental Engineering, The University of Western Ontario, London, ON N6A 5B9, Canada; [email protected]; Tel.: +1-519-661-4075 Received: 29 March 2020; Accepted: 20 April 2020; Published: 24 April 2020 Abstract: Global change, that results from population growth, global warming and land use change (especially rapid urbanization), is directly affecting the complexity of water resources management problems and the uncertainty to which they are exposed. Both, the complexity and the uncertainty, are the result of dynamic interactions between multiple system elements within three major systems: (i) the physical environment; (ii) the social environment; and (iii) the constructed infrastructure environment including pipes, roads, bridges, buildings, and other components. Recent trends in dealing with complex water resources systems include consideration of the whole region being affected, explicit incorporation of all costs and benefits, development of a large number of alternative solutions, and the active (early) involvement of all stakeholders in the decision-making. Systems approaches based on simulation, optimization, and multi-objective analyses, in deterministic, stochastic and fuzzy forms, have demonstrated in the last half of last century, a great success in supporting effective water resources management. This paper explores the future opportunities that will utilize advancements in systems theory that might transform management of water resources on a broader scale. The paper presents performance-based water resources engineering as a methodological framework to extend the role of the systems approach in improved sustainable water resources management under changing conditions (with special consideration given to rapid climate destabilization). -
Case Study: Water and Ice
Case Study: Water and Ice Timothy A. Isgro, Marcos Sotomayor, and Eduardo Cruz-Chu 1 The Universal Solvent Water is essential for sustaining life on Earth. Almost 75% of the Earth’s surface is covered by it. It composes roughly 70% of the human body by mass [1]. It is the medium associated with nearly all microscopic life pro- cesses. Much of the reason that water can sustain life is due to its unique properties. Among the most essential and extreme properties of water is its capabil- ity to absorb large amounts of heat. The heat capacity of water, which is the highest for compounds of its type in the liquid state, measures the amount of heat which needs to be added to water to change its temperature by a given amount. Water, thus, is able to effectively maintain its temperature even 1 when disturbed by great amounts of heat. This property serves to main- tain ocean temperatures, as well as the atmospheric temperature around the oceans. For example, when the sun rises in the morning and a large amount of heat strikes the surface of the Earth, the vast majority of it is absorbed by the ocean. The ocean water, however, does not exhibit a drastic increase in temperature that could make it inhospitable to life. In constrast, when the sun sets in the evening and that heat is taken away, the oceans do not become too cold to harbor life. Water also has high latent heats of vapor- ization and melting, which measure the amount of heat needed to change a certain amount of liquid water to vapor and ice to liquid, respectively. -
The Modelling of Freezing Process in Saturated Soil Based on the Thermal-Hydro-Mechanical Multi-Physics Field Coupling Theory
water Article The Modelling of Freezing Process in Saturated Soil Based on the Thermal-Hydro-Mechanical Multi-Physics Field Coupling Theory Dawei Lei 1,2, Yugui Yang 1,2,* , Chengzheng Cai 1,2, Yong Chen 3 and Songhe Wang 4 1 State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou 221008, China; [email protected] (D.L.); [email protected] (C.C.) 2 School of Mechanics and Civil Engineering, China University of Mining and Technology, Xuzhou 221116, China 3 State Key Laboratory of Coal Resource and Safe Mining, China University of Mining and Technology, Xuzhou 221116, China; [email protected] 4 Institute of Geotechnical Engineering, Xi’an University of Technology, Xi’an 710048, China; [email protected] * Correspondence: [email protected] Received: 2 September 2020; Accepted: 22 September 2020; Published: 25 September 2020 Abstract: The freezing process of saturated soil is studied under the condition of water replenishment. The process of soil freezing was simulated based on the theory of the energy and mass conservation equations and the equation of mechanical equilibrium. The accuracy of the model was verified by comparison with the experimental results of soil freezing. One-side freezing of a saturated 10-cm-high soil column in an open system with different parameters was simulated, and the effects of the initial void ratio, hydraulic conductivity, and thermal conductivity of soil particles on soil frost heave, freezing depth, and ice lenses distribution during soil freezing were explored. During the freezing process, water migrates from the warm end to the frozen fringe under the actions of the temperature gradient and pore pressure. -
Chapter 7 Seasonal Snow Cover, Ice and Permafrost
I Chapter 7 Seasonal snow cover, ice and permafrost Co-Chairmen: R.B. Street, Canada P.I. Melnikov, USSR Expert contributors: D. Riseborough (Canada); O. Anisimov (USSR); Cheng Guodong (China); V.J. Lunardini (USA); M. Gavrilova (USSR); E.A. Köster (The Netherlands); R.M. Koerner (Canada); M.F. Meier (USA); M. Smith (Canada); H. Baker (Canada); N.A. Grave (USSR); CM. Clapperton (UK); M. Brugman (Canada); S.M. Hodge (USA); L. Menchaca (Mexico); A.S. Judge (Canada); P.G. Quilty (Australia); R.Hansson (Norway); J.A. Heginbottom (Canada); H. Keys (New Zealand); D.A. Etkin (Canada); F.E. Nelson (USA); D.M. Barnett (Canada); B. Fitzharris (New Zealand); I.M. Whillans (USA); A.A. Velichko (USSR); R. Haugen (USA); F. Sayles (USA); Contents 1 Introduction 7-1 2 Environmental impacts 7-2 2.1 Seasonal snow cover 7-2 2.2 Ice sheets and glaciers 7-4 2.3 Permafrost 7-7 2.3.1 Nature, extent and stability of permafrost 7-7 2.3.2 Responses of permafrost to climatic changes 7-10 2.3.2.1 Changes in permafrost distribution 7-12 2.3.2.2 Implications of permafrost degradation 7-14 2.3.3 Gas hydrates and methane 7-15 2.4 Seasonally frozen ground 7-16 3 Socioeconomic consequences 7-16 3.1 Seasonal snow cover 7-16 3.2 Glaciers and ice sheets 7-17 3.3 Permafrost 7-18 3.4 Seasonally frozen ground 7-22 4 Future deliberations 7-22 Tables Table 7.1 Relative extent of terrestrial areas of seasonal snow cover, ice and permafrost (after Washburn, 1980a and Rott, 1983) 7-2 Table 7.2 Characteristics of the Greenland and Antarctic ice sheets (based on Oerlemans and van der Veen, 1984) 7-5 Table 7.3 Effect of terrestrial ice sheets on sea-level, adapted from Workshop on Glaciers, Ice Sheets and Sea Level: Effect of a COylnduced Climatic Change. -
Hydrated Sulfate Clusters SO4^2
Article Cite This: J. Phys. Chem. B 2019, 123, 4065−4069 pubs.acs.org/JPCB 2− n − Hydrated Sulfate Clusters SO4 (H2O)n ( =1 40): Charge Distribution Through Solvation Shells and Stabilization Maksim Kulichenko,† Nikita Fedik,† Konstantin V. Bozhenko,‡,§ and Alexander I. Boldyrev*,† † Department of Chemistry and Biochemistry, Utah State University, 0300 Old Main Hill, Logan, Utah 84322-0300, United States ‡ Department of Physical and Colloid Chemistry, Peoples’ Friendship University of Russia (RUDN University), 6 Miklukho-Maklaya St, Moscow 117198, Russian Federation § Institute of Problems of Chemical Physics, Russian Academy of Sciences, Chernogolovka 142432, Moscow Region, Russian Federation *S Supporting Information 2− ABSTRACT: Investigations of inorganic anion SO4 interactions with water are crucial 2− for understanding the chemistry of its aqueous solutions. It is known that the isolated SO4 dianion is unstable, and three H2O molecules are required for its stabilization. In the 2− current work, we report our computational study of hydrated sulfate clusters SO4 (H2O)n (n =1−40) in order to understand the nature of stabilization of this important anion by fi 2− water molecules. We showed that the most signi cant charge transfer from dianion SO4 ≤ 2− to H2O takes place at a number of H2O molecules n 7. The SO4 directly donates its charge only to the first solvation shell and surprisingly, a small amount of electron density of 0.15|e| is enough to be transferred in order to stabilize the dianion. Upon further addition of ff ≤ H2O molecules, we found that the cage e ect played an essential role at n 12, where the fi 2− | | rst solvation shell closes. -
Freshwater Resources
3 Freshwater Resources Coordinating Lead Authors: Blanca E. Jiménez Cisneros (Mexico), Taikan Oki (Japan) Lead Authors: Nigel W. Arnell (UK), Gerardo Benito (Spain), J. Graham Cogley (Canada), Petra Döll (Germany), Tong Jiang (China), Shadrack S. Mwakalila (Tanzania) Contributing Authors: Thomas Fischer (Germany), Dieter Gerten (Germany), Regine Hock (Canada), Shinjiro Kanae (Japan), Xixi Lu (Singapore), Luis José Mata (Venezuela), Claudia Pahl-Wostl (Germany), Kenneth M. Strzepek (USA), Buda Su (China), B. van den Hurk (Netherlands) Review Editor: Zbigniew Kundzewicz (Poland) Volunteer Chapter Scientist: Asako Nishijima (Japan) This chapter should be cited as: Jiménez Cisneros , B.E., T. Oki, N.W. Arnell, G. Benito, J.G. Cogley, P. Döll, T. Jiang, and S.S. Mwakalila, 2014: Freshwater resources. In: Climate Change 2014: Impacts, Adaptation, and Vulnerability. Part A: Global and Sectoral Aspects. Contribution of Working Group II to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Field, C.B., V.R. Barros, D.J. Dokken, K.J. Mach, M.D. Mastrandrea, T.E. Bilir, M. Chatterjee, K.L. Ebi, Y.O. Estrada, R.C. Genova, B. Girma, E.S. Kissel, A.N. Levy, S. MacCracken, P.R. Mastrandrea, and L.L. White (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp. 229-269. 229 Table of Contents Executive Summary ............................................................................................................................................................ 232 3.1. Introduction ...........................................................................................................................................................