Evaluating Lake Response to Environmental and Climatic Change Using Lake Core Records and Modeling

Total Page:16

File Type:pdf, Size:1020Kb

Evaluating Lake Response to Environmental and Climatic Change Using Lake Core Records and Modeling University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Earth and Atmospheric Sciences, Department Atmospheric Sciences of 2009 Evaluating Lake Response to Environmental and Climatic Change using Lake Core Records and Modeling Brandi Bracht-Flyr University of Nebraska at Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons Bracht-Flyr, Brandi, "Evaluating Lake Response to Environmental and Climatic Change using Lake Core Records and Modeling" (2009). Dissertations & Theses in Earth and Atmospheric Sciences. 4. https://digitalcommons.unl.edu/geoscidiss/4 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. EVALUATING LAKE RESPONSE TO ENVIRONMENTAL AND CLIMATIC CHANGE USING LAKE CORE RECORDS AND MODELING by Brandi B. Bracht-Flyr A DISSERTATION Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfilment of Requirements For the Degree of Doctor of Philosophy Major: Geosciences (Geology) Under the Supervision of Professor Sherilyn C. Fritz Lincoln, Nebraska November, 2009 EVALUATING LAKE RESPONSE TO ENVIRONMENTAL AND CLIMATIC CHANGE USING LAKE CORE RECORDS AND MODELING Brandi B. Bracht-Flyr, Ph.D University of Nebraska, 2009 Adviser: Sherilyn C. Frtiz This dissertation evaluates how lakes respond to changes in their environmental and climatic settings. This dissertation consists of two lake modeling projects and the environ- mental and paleoclimatic reconstructions of four lakes in southwestern Montana. Lakes and their associated biological communities respond to environmental and climatic change on rapid timescales. Lake modeling and lake core stratigraphies are complementary tools for exploration of how lakes and their biota respond to environmental or climatic perturba- tions. In one modeling approach for exploring these issues, a simple hydro-climatological lake model was developed that classifies lake sensitivity to climatic perturbations based upon lake area, catchment area, precipitation, and evapotranspiration. Using simple ratios of these commonly measured parameters the model classifies lakes into three domains: ephemeral, sensitive to vegetation change, and permanent. The lakes that plot within the sensitive to vegetation change domain should show water balance fluctuations in response to environmental change, and these lakes would make good targets for paleoclimatic stud- ies. Diatom records from four lakes, Crevice Lake, Foy Lake, Morrison Lake, and Reser- voir Lake, in southwestern Montana provide late-Holocene (past 3000 years) records of environmental and climatic variability. The lakes show similarities in the timing of major changes in the fossil diatom assemblages, suggesting regional climate forcings. Spectral analysis of the lake-core records suggest periodic fluctuations at spectral frequencies that are characteristic of oceanic influence on climate, such as the Atlantic Multi-decadal Os- cillation and Pacific Decadal Oscillation. The Crevice Lake core diatom record shows three distinctive diatom communities dur- ing the approximately the last 1000 years. The model DYRESM-CAEDYM was used in an inverse modeling approach to provide a means to estimate climate variables during these three stages. The model estimates of climate variables during the Medieval Period, the Little Ice Age, and the 20th century, include incoming shortwave radiation, cloud cover, vapor pressure, and wind speed. The model results suggests that changes in spring sea- sonality, when the climate variables differ the most, is more important in affecting diatom community composition than total deviations from modern averages. iv DEDICATION I would like to dedicate this dissertation to my wonderful husband, Mike, whose support and laughter kept me sane throughout this entire process. Also, to my parents, Gary and Vicki Bracht, who have never questioned my dreams, or career choice. v ACKNOWLEDGMENTS First and foremost, I would like to acknowledge and thank my advisor, Dr. Sherilyn Fritz for her all her assistance, and for putting up with my writing. I would like to thank the University of Nebraska-Lincoln Department of Geosciences and the Geological Society of America for providing funding and grant assistance. I would like to thank my committee, Dr. Kyle Hoagland, Dr. Robert Oglesby, Dr. John Lenters, and Dr. John Gates for their support and critique of my research efforts. Jeffery Stone and Karlyn Westover sparked my interest in the lake and paleoclimate realm. Without their willingness to teach and friendship, I am not sure I would be at the point I am now. Dr. Eric Grimm and Pietra Mueller cored both Reservoir and Morrison Lakes and provided assistance sampling the cores. The Yellowstone National Park Research Office, particularly Christie Hendrix and Stacey Gunther, provided assistance with field work and research permitting. Gary, Vicki, and Blake Bracht were always willing to assist in field work, regardless of how far I made them hike. I am extremely grateful to all those who helped, in a myriad of ways, to make this dream possible. vi Contents Contents vi List of Figuresx List of Tables xii 1 Introduction1 1.1 Background & Scope............................. 2 1.2 Preface To Chapters.............................. 4 1.2.1 Chapter 2............................... 4 1.2.2 Chapter 3............................... 5 1.2.3 Chapter 4............................... 6 1.2.4 Chapter 5............................... 6 References7 2 A hydro-climatological lake classification model and its evaluation using data9 2.1 Introduction.................................. 11 2.2 Methods.................................... 13 2.2.1 Analytical Model........................... 13 2.2.2 Data.................................. 19 vii 2.3 Results..................................... 21 2.4 Discussion................................... 23 2.5 Conclusion .................................. 28 References 35 3 Synchronous late-Holocene climatic change inferred from four western Mon- tana lakes 43 3.1 Introduction.................................. 44 3.1.1 Environmental Setting ........................ 45 3.1.2 Climatic Setting............................ 47 3.2 Methods.................................... 49 3.2.1 Coring................................. 49 3.2.2 Diatoms & Geochemistry....................... 50 3.2.3 Age Models.............................. 50 3.2.4 Statistical Techniques......................... 51 3.3 Results..................................... 53 3.3.1 Lithology & Geochemistry...................... 53 3.3.2 DCA Results ............................. 53 3.3.3 Spectral Analysis Results....................... 54 3.4 Discussion................................... 55 3.4.1 Limnological History......................... 55 3.4.2 Regional Patterns........................... 62 3.4.3 Forcing of Regional Climate Change................. 65 3.5 Conclusion .................................. 67 References 69 viii 4 Combining lake core records with the limnologic model DYRESM-CAEDYM to estimate climatic parameters during the Little Ice Age and Medieval Warm Period 76 4.1 Introduction.................................. 77 4.1.1 Study Area .............................. 79 4.1.2 Crevice Lake History & Ecology................... 80 4.1.3 DYRESM-CAEDYM......................... 82 4.2 Methods.................................... 83 4.2.1 Weather Data & Lake Temperature.................. 83 4.2.2 Model Setup.............................. 84 4.2.3 Development of LIA and MWP Weather Data............ 85 4.3 Results..................................... 87 4.3.1 Field Data............................... 87 4.3.2 Model Simulations .......................... 87 4.4 Discussion................................... 98 4.4.1 Contemporary Scenario........................ 99 4.4.2 LIA ..................................100 4.4.3 MWP .................................101 4.4.4 Seasonality Effects ..........................101 4.4.5 Model Limitations ..........................102 4.5 Conclusions..................................103 References 105 5 Summary 110 5.1 Conclusions..................................111 5.1.1 Major Findings............................111 ix 5.1.2 Suggestions for Further Research...................112 x List of Figures 2.1 Lake-climate conceptual model.......................... 17 2.2 Locality map ................................... 19 2.3 Lake model .................................... 22 3.1 Map of study area................................. 46 3.2 Lake bathymetric maps.............................. 48 3.3 Lake age models ................................. 51 3.4 Lake DCA results................................. 54 3.5 Lake spectral analysis results........................... 55 3.6 Crevice Lake diatom stratigraphy......................... 57 3.7 Foy Lake diatom stratigraphy........................... 59 3.8 Morrison Lake diatom stratigraphy........................ 60 3.9 Reservoir Lake diatom stratigraphy........................ 61 3.10 Schematic diagram ................................ 64 4.1 Crevice Lake locality map ............................ 79 4.2 Crevice Lake diatom stratigraphy........................
Recommended publications
  • Petition to List US Populations of Lake Sturgeon (Acipenser Fulvescens)
    Petition to List U.S. Populations of Lake Sturgeon (Acipenser fulvescens) as Endangered or Threatened under the Endangered Species Act May 14, 2018 NOTICE OF PETITION Submitted to U.S. Fish and Wildlife Service on May 14, 2018: Gary Frazer, USFWS Assistant Director, [email protected] Charles Traxler, Assistant Regional Director, Region 3, [email protected] Georgia Parham, Endangered Species, Region 3, [email protected] Mike Oetker, Deputy Regional Director, Region 4, [email protected] Allan Brown, Assistant Regional Director, Region 4, [email protected] Wendi Weber, Regional Director, Region 5, [email protected] Deborah Rocque, Deputy Regional Director, Region 5, [email protected] Noreen Walsh, Regional Director, Region 6, [email protected] Matt Hogan, Deputy Regional Director, Region 6, [email protected] Petitioner Center for Biological Diversity formally requests that the U.S. Fish and Wildlife Service (“USFWS”) list the lake sturgeon (Acipenser fulvescens) in the United States as a threatened species under the federal Endangered Species Act (“ESA”), 16 U.S.C. §§1531-1544. Alternatively, the Center requests that the USFWS define and list distinct population segments of lake sturgeon in the U.S. as threatened or endangered. Lake sturgeon populations in Minnesota, Lake Superior, Missouri River, Ohio River, Arkansas-White River and lower Mississippi River may warrant endangered status. Lake sturgeon populations in Lake Michigan and the upper Mississippi River basin may warrant threatened status. Lake sturgeon in the central and eastern Great Lakes (Lake Huron, Lake Erie, Lake Ontario and the St. Lawrence River basin) seem to be part of a larger population that is more widespread.
    [Show full text]
  • Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a Foundation in Northern Manitoba
    Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba Karla Zubrycki Dimple Roy Hisham Osman Kimberly Lewtas Geoffrey Gunn Richard Grosshans © 2014 The International Institute for Sustainable Development © 2016 International Institute for Sustainable Development | IISD.org November 2016 Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba © 2016 International Institute for Sustainable Development Published by the International Institute for Sustainable Development International Institute for Sustainable Development The International Institute for Sustainable Development (IISD) is one Head Office of the world’s leading centres of research and innovation. The Institute provides practical solutions to the growing challenges and opportunities of 111 Lombard Avenue, Suite 325 integrating environmental and social priorities with economic development. Winnipeg, Manitoba We report on international negotiations and share knowledge gained Canada R3B 0T4 through collaborative projects, resulting in more rigorous research, stronger global networks, and better engagement among researchers, citizens, Tel: +1 (204) 958-7700 businesses and policy-makers. Website: www.iisd.org Twitter: @IISD_news IISD is registered as a charitable organization in Canada and has 501(c)(3) status in the United States. IISD receives core operating support from the Government of Canada, provided through the International Development Research Centre (IDRC) and from the Province
    [Show full text]
  • Weekly Update #7 – February 21, 2020
    Water Level & Flow Update for the Lower Nelson River Weekly Update # 7 February 21, 2020 Lower Nelson River (Split Lake to Hudson Bay) Water up and impoundment has not started at Keeyask (planned to begin in February). Flows on the Nelson River are high as heavy Fall rainfall in the southern parts of the watershed flows north on its way to Hudson Bay - this will continue all winter. Hydro system flows to Split Lake and the Lower Nelson River come from 2 sources – Lake Winnipeg (LW) outflows through Kelsey generating station (at 3115 cms or 110,000 cfs) and Churchill River Diversion (CRD), through Notigi control structure (960 cms or 33,900 cfs)-see map. These combined flows (of 4,075 cms or 143,900 cfs) have been relatively constant since early December. The Nelson’s flow downstream of Keeyask is 4,480 cms ( or 158,200 cfs) (measured at As of February 19, Lower Nelson River lake and Limestone GS). forebay levels are: • Split Lake 168.35 m (or 552.3 ft) Nelson River flow depends on Lake Winnipeg Water level: • Clark Lake 167.94 m (or 551.0 ft ) Lake Winnipeg outflows are largely controlled by the • Gull Lake 156.17 m (or 512.4 ft ) Jenpeg Generating Station (upstream of Kelsey Jenpeg• Stephens Lake 139.76 m (or 458.5 ft) Generating Station). These flows are maximized every • Long Spruce forebay 110.90 m (or 361.2 ft ) winter to allow as much water as possible to flow out of • Limestone forebay 85.07 m (or 279.1 ft) Lake Winnipeg to fuel generating stations on the Nelson River to meet heating demands by Manitobans.
    [Show full text]
  • Convergent Margin Magmatism in the Central Andes and Its Near Antipodes in Western Indonesia: Spatiotemporal and Geochemical Considerations
    AN ABSTRACT OF THE DISSERTATION OF Morgan J. Salisbury for the degree of Doctor of Philosophy in Geology presented on June 3, 2011. Title: Convergent Margin Magmatism in the Central Andes and its Near Antipodes in Western Indonesia: Spatiotemporal and Geochemical Considerations Abstract approved: ________________________________________________________________________ Adam J.R. Kent This dissertation combines volcanological research of three convergent continental margins. Chapters 1 and 5 are general introductions and conclusions, respectively. Chapter 2 examines the spatiotemporal development of the Altiplano-Puna volcanic complex in the Lípez region of southwest Bolivia, a locus of a major Neogene ignimbrite flare- up, yet the least studied portion of the Altiplano-Puna volcanic complex of the Central Andes. New mapping and laser-fusion 40Ar/39Ar dating of sanidine and biotite from 56 locations, coupled with paleomagnetic data, refine the timing and volumes of ignimbrite emplacement in Bolivia and northern Chile to reveal that monotonous intermediate volcanism was prodigious and episodic throughout the complex. 40Ar/39Ar age determinations of 13 ignimbrites from northern Chile previously dated by the K-Ar method improve the overall temporal resolution of Altiplano-Puna volcanic complex development. Together with new and updated volume estimates, the new age determinations demonstrate a distinct onset of Altiplano-Puna volcanic complex ignimbrite volcanism with modest output rates beginning ~11 Ma, an episodic middle phase with the highest eruption rates between 8 and 3 Ma, followed by a general decline in volcanic output. The cyclic nature of individual caldera complexes and the spatiotemporal pattern of the volcanic field as a whole are consistent with both incremental construction of plutons as well as a composite Cordilleran batholith.
    [Show full text]
  • A Freshwater Classification of the Mackenzie River Basin
    A Freshwater Classification of the Mackenzie River Basin Mike Palmer, Jonathan Higgins and Evelyn Gah Abstract The NWT Protected Areas Strategy (NWT-PAS) aims to protect special natural and cultural areas and core representative areas within each ecoregion of the NWT to help protect the NWT’s biodiversity and cultural landscapes. To date the NWT-PAS has focused its efforts primarily on terrestrial biodiversity, and has identified areas, which capture only limited aspects of freshwater biodiversity and the ecological processes necessary to sustain it. However, freshwater is a critical ecological component and physical force in the NWT. To evaluate to what extent freshwater biodiversity is represented within protected areas, the NWT-PAS Science Team completed a spatially comprehensive freshwater classification to represent broad ecological and environmental patterns. In conservation science, the underlying idea of using ecosystems, often referred to as the coarse-filter, is that by protecting the environmental features and patterns that are representative of a region, most species and natural communities, and the ecological processes that support them, will also be protected. In areas such as the NWT where species data are sparse, the coarse-filter approach is the primary tool for representing biodiversity in regional conservation planning. The classification includes the Mackenzie River Basin and several watersheds in the adjacent Queen Elizabeth drainage basin so as to cover the ecoregions identified in the NWT-PAS Mackenzie Valley Five-Year Action Plan (NWT PAS Secretariat 2003). The approach taken is a simplified version of the hierarchical classification methods outlined by Higgins and others (2005) by using abiotic attributes to characterize the dominant regional environmental patterns that influence freshwater ecosystem characteristics, and their ecological patterns and processes.
    [Show full text]
  • Sediment Records of the Influence of River Damming on the Dynamics Of
    HOL0010.1177/0959683616670465The HoloceneDuboc et al. 670465research-article2016 Research paper The Holocene 2017, Vol. 27(5) 712 –725 Sediment records of the influence of river © The Author(s) 2016 Reprints and permissions: sagepub.co.uk/journalsPermissions.nav damming on the dynamics of the Nelson DOI:https://doi.org/10.1177/0959683616670465 10.1177/0959683616670465 and Churchill Rivers, western Hudson Bay, journals.sagepub.com/home/hol Canada, during the last centuries Quentin Duboc,1,2 Guillaume St-Onge1,2 and Patrick Lajeunesse3 Abstract Two gravity cores (778 and 780) sampled at the Nelson River mouth and one (776) at the Churchill River mouth in western Hudson Bay, Canada, were analyzed in order to identify the impact of dam construction on hydrology and sedimentary regime of both rivers. Another core (772) was sampled offshore and used as a reference core without a direct river influence. Core chronology was established using 14C and 210Pb measurements. Cores 778 and 780 show greater variability than the others, and the physical, chemical, magnetic, and sedimentological properties measured on these cores reveal the presence of several hyperpycnites, indicating the occurrence of hyperpycnal flows associated with floods of the Nelson River. These hyperpycnal flows were probably caused by ice-jam formation, which can increase both the flow and the sediment concentration following the breaching of such natural dams. However, these hyperpycnites are only observed in the lower parts of cores 778 and 780. It was not possible to establish a precise chronology because of the remobilization of sediments by the floods. Nevertheless, some modern 14C ages suggest that this change in sedimentary regime is recent and could be concurrent with the dam construction on the Nelson River, which allows a continuous control of its flow since the 1960s.
    [Show full text]
  • Lake Agassiz: a Chapter in Glacial Geology
    Journal of the Minnesota Academy of Science Volume 2 Number 4 Article 5 1883 Lake Agassiz: A Chapter in Glacial Geology Warren Upham Follow this and additional works at: https://digitalcommons.morris.umn.edu/jmas Part of the Geology Commons, and the Glaciology Commons Recommended Citation Upham, W. (1883). Lake Agassiz: A Chapter in Glacial Geology. Journal of the Minnesota Academy of Science, Vol. 2 No.4, 290-314. Retrieved from https://digitalcommons.morris.umn.edu/jmas/vol2/iss4/5 This Article is brought to you for free and open access by the Journals at University of Minnesota Morris Digital Well. It has been accepted for inclusion in Journal of the Minnesota Academy of Science by an authorized editor of University of Minnesota Morris Digital Well. For more information, please contact [email protected]. LAK;E AGASSIZ : A . CHAPTER IN GLACIAL GEOLOGY. BY WARREN tTPIUM• • In tha last ol the geological ages a "'lery cold climate cov~ (!red the north part of our continent wfth ice. Every year the snowfall was greater than could be melted away in sum­ mer; and its depth gradually increased till its lower portion Was changed to compact ice by the pressure of its weight. This pressure also caused the "'last sheet of ice to moYe slowly outward. from the region of its greatest thickness toward its margin. Our reasons for believing that there has been such a wonderful glacial period, are abundant and must convince anyone who gi"'les attention to them. The surfaces of the bed-rock at the quarries in this city, on Nicollet island and beside the Mississippi farther east, bear fine scratches and markings, called stn:m, like those which are found beneath the glaciers of the Alps.
    [Show full text]
  • Cec-Decision-Pimicikamak.Pdf
    The Manitoba Clean Environment Commission Pimicikamak Cree Nation Motion Respecting: The Wuskwatim Generation and Transmission Project Background In April 2003, Manitoba Hydro (“Hydro”) and the Nisichawayasihk Cree Nation (“NCN”) filed Environmental Impact Statements and the Justification, Need for and Alternatives to the proposed Wuskwatim Generation Project with the Manitoba Clean Environment Commission (“CEC”). Also, in April 2003 Hydro filed Environmental Impact Statements and the Justification, Need for and Alternatives to the proposed Wuskwatim Transmission Project with the CEC. These two filings constitute (“the Filing”). On August 28, 2003, the CEC set out a Preliminary Pre-Hearing Schedule to conduct a review of the Filing which provides an opportunity for all interested parties to submit information requests, file evidence prior to the hearing, conduct cross examination, and submit final argument at the hearing. On July 28, 2003, the CEC received a motion from the Pimicikamak Cree Nation (“PCN”) regarding the Filing. In addition to accepting written responses to the PCN motion from Hydro and NCN, the CEC received written comments from other interested parties and held a hearing on September 30, 2003 to listen to oral argument regarding the PCN motion. Oral and written submissions were provided by PCN, Hydro, NCN, the Association for the Displaced Residents of South Indian Lake (“DRSIL”), the Boreal Forest Network (“BFN”), the Canadian Nature Federation (“CNF”), the Community Association of South Indian Lake (“CASIL”), the Consumers Association of Canada/Manitoba Society of Seniors (“CAC/MSOS”), the O-Pipon-Na-Piwin Cree Nation (“OCN”), the Tataskweyak Cree Nation (“TCN”), Time to Respect Earth’s Ecosystem/Resource Conservation Manitoba (“TREE/RCM”), Trapline #18, and Manitoba Conservation.
    [Show full text]
  • Glaciers of the Canadian Rockies
    Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES By C. SIMON L. OMMANNEY SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The Rocky Mountains of Canada include four distinct ranges from the U.S. border to northern British Columbia: Border, Continental, Hart, and Muskwa Ranges. They cover about 170,000 km2, are about 150 km wide, and have an estimated glacierized area of 38,613 km2. Mount Robson, at 3,954 m, is the highest peak. Glaciers range in size from ice fields, with major outlet glaciers, to glacierets. Small mountain-type glaciers in cirques, niches, and ice aprons are scattered throughout the ranges. Ice-cored moraines and rock glaciers are also common CONTENTS Page Abstract ---------------------------------------------------------------------------- J199 Introduction----------------------------------------------------------------------- 199 FIGURE 1. Mountain ranges of the southern Rocky Mountains------------ 201 2. Mountain ranges of the northern Rocky Mountains ------------ 202 3. Oblique aerial photograph of Mount Assiniboine, Banff National Park, Rocky Mountains----------------------------- 203 4. Sketch map showing glaciers of the Canadian Rocky Mountains -------------------------------------------- 204 5. Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August 1973 -------------------------------------- 209 TABLE 1. Named glaciers of the Rocky Mountains cited in the chapter
    [Show full text]
  • Aeolian Processes and the Biosphere
    AEOLIAN PROCESSES AND THE BIOSPHERE Sujith Ravi,1 Paolo D’Odorico,2 David D. Breshears,3 Jason P. Field,3 Andrew S. Goudie,4 Travis E. Huxman,1 Junran Li,5,6 Gregory S. Okin,6 Robert J. Swap,2 Andrew D. Thomas,7 Scott Van Pelt,8 Jeffrey J. Whicker,9 and Ted M. Zobeck10 Received 3 January 2010; revised 22 February 2011; accepted 18 April 2011; published 3 August 2011. [1] Aeolian processes affect the biosphere in a wide variety at a variety of scales, including large‐scale dust transport of contexts, including landform evolution, biogeochemical and global biogeochemical cycles, climate mediated interac- cycles, regional climate, human health, and desertification. tions between atmospheric dust and ecosystems, impacts on Collectively, research on aeolian processes and the bio- human health, impacts on agriculture, and interactions sphere is developing rapidly in many diverse and specialized between aeolian processes and dryland vegetation. Aeolian areas, but integration of these recent advances is needed to dust emissions are driven largely by, in addition to climate, better address management issues and to set future research a combination of soil properties, soil moisture, vegetation priorities. Here we review recent literature on aeolian pro- and roughness, biological and physical crusts, and distur- cesses and their interactions with the biosphere, focusing bances. Aeolian research methods span laboratory and field on (1) geography of dust emissions, (2) impacts, interactions, techniques, modeling, and remote sensing. Together these and feedbacks, (3) drivers of dust emissions, and (4) method- integrated perspectives on aeolian processes and the bio- ological approaches. Geographically, dust emissions are sphere provide insights into management options and aid highly spatially variable but also provide connectivity at in identifying research priorities, both of which are increas- global scales between sources and effects, with “hot spots” ingly important given that global climate models predict an being of particular concern.
    [Show full text]
  • Water Level & Flow Update for the Lower Nelson River
    Water Level & Flow Update for the Lower Nelson River Weekly Update # 9 March 6 2020 Lower Nelson River (Split Lake to Hudson Bay) Watering up activities started at Keeyask on February 26, 2020. Flows on the Nelson River are high as heavy Fall rainfall in the southern parts of the watershed flows north on its way to Hudson Bay - this will continue all winter. Hydro system flows to Split Lake and the Lower Nelson River come from 2 sources – Lake Winnipeg (LW) outflows through Kelsey generating station (at 3150 cms or 111,200 cfs) and Churchill River Diversion (CRD), through Notigi control structure (955 cms or 33,700 cfs).. These combined flows of 4,105 cms (or 145,000 cfs) have been relatively constant since early December. The Nelson’s flow downstream of Keeyask is 4,200 cms (or 158,300 cfs) As of March 4, Lower Nelson River lake and (measured at Limestone GS). (See Map) forebay levels are: • Split Lake 168.10 m (or 551.5 ft) Nelson River flow depends on Lake Winnipeg Water level: • Clark Lake 167.63 m (or 550.0 ft ) Lake Winnipeg outflows are largely controlled by the • Gull Lake 156.41 m (or 513.2 ft ) Jenpeg Generating Station (upstream of Kelsey Jenpeg• Stephens Lake 140.33 m (or 460.4 ft) Generating Station). These flows are maximized every • Long Spruce forebay 109.95 m (or 360.7 ft ) winter to allow as much water as possible to flow out of • Limestone forebay 84.98 m (or 278.8 ft) Lake Winnipeg to fuel generating stations on the Nelson River to meet heating demands by Manitobans.
    [Show full text]
  • The Early Wisconsinan History of the Laurentide Ice Sheet
    Document generated on 10/05/2021 2:08 a.m. Géographie physique et Quaternaire The Early Wisconsinan History of the Laurentide Ice Sheet L’évolution de la calotte glaciaire laurentidienne au Wisconsinien inférieur Geschichte der laurentischen Eisdecke im frühen glazialen Wisconsin Jean-Serge Vincent and Victor K. Prest La calotte glaciaire laurentidienne Article abstract The Laurentide Ice Sheet The identification, particularly at the periphery of the ice sheet, of glacigenic Volume 41, Number 2, 1987 sediments thought to postdate nonglacial sediments or paleosols regarded as having been laid down sometime during the Sangamonian Interglaciation URI: https://id.erudit.org/iderudit/032679ar (stage 5) and thought to predate nonglacial sediments or soils reckoned to be of DOI: https://doi.org/10.7202/032679ar Middle Wisconsinan age (stage 3), has led numerous authors to propose that the Laurentide Ice Sheet initially grew during the Sangamonian and/or the Early Wisconsinan (stage 4). The evidence for the beginning of the See table of contents Wisconsinan ice sheet in various areas of Canada and the northern United States is briefly reviewed. The general absence of sound geochronometric frameworks for potential Sangamonian or Early Wisconsinan glacial deposits Publisher(s) has led to a situation where in most areas it can be argued, depending on one's interpretation, that ice completely inundated or was completely absent at that Les Presses de l'Université de Montréal time. On the premise (perhaps false) that Laurentide Ice was in fact extensive during the Early Wisconsinan, a map showing maximum possible ice extent, as ISSN put forward by some authors is presented and the glacigenic units possibly 0705-7199 (print) recording the ice advance are shown in a correlation chart.
    [Show full text]