Modeling and Management Option Analysis for Saline Groundwater Drainage in a Deltaic Island
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15 NOVEMBER 2006 A R O R A A N D B O E R 5875 The Temporal Variability of Soil Moisture and Surface Hydrological Quantities in a Climate Model VIVEK K. ARORA AND GEORGE J. BOER Canadian Centre for Climate Modelling and Analysis, Meteorological Service of Canada, University of Victoria, Victoria, British Columbia, Canada (Manuscript received 4 October 2005, in final form 8 February 2006) ABSTRACT The variance budget of land surface hydrological quantities is analyzed in the second Atmospheric Model Intercomparison Project (AMIP2) simulation made with the Canadian Centre for Climate Modelling and Analysis (CCCma) third-generation general circulation model (AGCM3). The land surface parameteriza- tion in this model is the comparatively sophisticated Canadian Land Surface Scheme (CLASS). Second- order statistics, namely variances and covariances, are evaluated, and simulated variances are compared with observationally based estimates. The soil moisture variance is related to second-order statistics of surface hydrological quantities. The persistence time scale of soil moisture anomalies is also evaluated. Model values of precipitation and evapotranspiration variability compare reasonably well with observa- tionally based and reanalysis estimates. Soil moisture variability is compared with that simulated by the Variable Infiltration Capacity-2 Layer (VIC-2L) hydrological model driven with observed meteorological data. An equation is developed linking the variances and covariances of precipitation, evapotranspiration, and runoff to soil moisture variance via a transfer function. The transfer function is connected to soil moisture persistence in terms of lagged autocorrelation. Soil moisture persistence time scales are shorter in the Tropics and longer at high latitudes as is consistent with the relationship between soil moisture persis- tence and the latitudinal structure of potential evaporation found in earlier studies. -
Why Do We Have So Many Different Hydrological Models?
Why do we have so many different hydrological models? A review based on the case of Switzerland Pascal Horton*1, Bettina Schaefli1, and Martina Kauzlaric1 1Institute of Geography & Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland ([email protected]) This is a preprint of a manuscript submitted to WIREs Water. 1 Abstract Hydrology plays a central role in applied as well as fundamental environmental sciences, but it is well known to suffer from an overwhelming diversity of models, in particular to simulate streamflow. Based on Switzerland's example, we discuss here in detail how such diversity did arise even at the scale of such a small country. The case study's relevance stems from the fact that Switzerland shows a relatively high density of academic and research institutes active in the field of hydrology, which led to an evolution of hydrological models that stands exemplarily for the diversification that arose at a larger scale. Our analysis summarizes the main driving forces behind this evolution, discusses drawbacks and advantages of model diversity and depicts possible future evolutions. Although convenience seems to be the main driver so far, we see potential change in the future with the advent of facilitated collaboration through open sourcing and code sharing platforms. We anticipate that this review, in particular, helps researchers from other fields to understand better why hydrologists have so many different models. 1 Introduction Hydrological models are essential tools for hydrologists, be it for operational flood forecasting, water resource management or the assessment of land use and climate change impacts. -
District Sl No Name Post Present Place of Posting S 24 Pgs 1 TANIA
District Sl No Name Post Present Place of Posting PADMERHAT RURAL S 24 Pgs 1 TANIA SARKAR GDMO HOSPITAL S 24 Pgs 2 DR KIRITI ROY GDMO HARIHARPUR PHC S 24 Pgs 3 Dr. Monica Chattrejee, GDMO Kalikapur PHC S 24 Pgs 4 Dr. Debasis Chakraborty, GDMO Sonarpur RH S 24 Pgs 5 Dr. Tusar Kanti Ghosh, GDMO Fartabad PHC S 24 Pgs 6 Dr. Iman Bhakta GDMO Kalikapur PHC Momrejgarh PHC, Under S 24 Pgs 7 Dr. Uday Sankar Koyal GDMO Padmerhat RH, Joynagar - I Block S 24 Pgs 8 Dr. Dipak Kumar Ray GDMO Nolgara PHC S 24 Pgs 9 Dr. Basudeb Kar GDMO Jaynagar R.H. S 24 Pgs 10 Dr. Amitava Chowdhury GDMO Jaynagar R.H. Dr. Sambit Kumar S 24 Pgs 11 GDMO Jaynagar R.H. Mukharjee Nalmuri BPHC,Bhnagore S 24 Pgs 12 Dr. Snehadri Nayek GDMO I Block,S 24 Pgs Jirangacha S 24 Pgs 13 Dr. Shyama pada Banarjee GDMO BPHC(bhangar-II Block) Jirangacha S 24 Pgs 14 Dr. Himadri sekhar Mondal GDMO BPHC(bhangar-II Block) S 24 Pgs 15 Dr. Tarek Anowar Sardar GDMO Basanti BPHC S 24 Pgs 16 Debdeep Ghosh GDMO Basanti BPHC S 24 Pgs 17 Dr.Nitya Ranjan Gayen GDMO Jharkhali PHC S 24 Pgs 18 GDMO SK NAWAZUR RAHAMAN GHUTARI SARIFF PHC S 24 Pgs 19 GDMO DR. MANNAN ZINNATH GHUTARI SARIFF PHC S 24 Pgs 20 Dr.Manna Mondal GDMO Gosaba S 24 Pgs 21 Dr. Aminul Islam Laskar GDMO Matherdighi BPHC S 24 Pgs 22 Dr. Debabrata Biswas GDMO Kuchitalahat PHC S 24 Pgs 23 Dr. -
Hydrological Induced Earth Rotation Variations from Stand-Alone and Dynamically Coupled Simulations
HYDROLOGICAL INDUCED EARTH ROTATION VARIATIONS FROM STAND-ALONE AND DYNAMICALLY COUPLED SIMULATIONS R. DILL, M. THOMAS, C. WALTER Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences Telegrafenberg, D-14473 Potsdam e-mail: [email protected] ABSTRACT. The impact of continental water mass redistributions on Earth rotation is deduced from stand-alone runs with the Hydrological Discharge Model (HDM) forced by ERA40 re-analyses as well as by the unconstrained atmospheric climate model ECHAM5. The HDM is attached in three different approaches to the atmospheric forcing models. First, ECHAM5 and its embedded land surface model generates directly runoff and drainage appropriate for the subsequent processing with HDM, like it is re- alized in the dynamically coupled model system ECOCTH, too. Second, an intermediate Simplified Land Surface scheme (SLS) is used to separate ERA40 precipitation into runoff, drainage, and evaporation. Third, precipitation and evaporation are used as input for the Land Surface Discharge Model (LSDM), which estimates runoff and drainage internally for its HDM-like discharge scheme. The individual models are validated by observed river discharges. The induced rotational variations represent mainly the dif- ferent forcing from precipitation-evaporation and trends from inconsistent mass fluxes. The dynamical coupling of atmosphere and ocean has only a subordinated influence. 1. HYDROLOGICAL MODEL APPROACHES Water mass redistributions within the global hydrological cycle affect the Earth’s rotation and its gravity field, especially on seasonal to interannual timescales. Since Earth rotation variations and partic- ularly Length-of-Day are sensitive for deficiencies in the global water balance, consistent mass exchanges among the atmosphere, oceans and continental hydrology are mandatory for realistic simulations of hy- drospheric induced global integral Earth parameters. -
Hydrological Controls on Salinity Exposure and the Effects on Plants in Lowland Polders
Hydrological controls on salinity exposure and the effects on plants in lowland polders Sija F. Stofberg Thesis committee Promotors Prof. Dr S.E.A.T.M. van der Zee Personal chair Ecohydrology Wageningen University & Research Prof. Dr J.P.M. Witte Extraordinary Professor, Faculty of Earth and Life Sciences, Department of Ecological Science VU Amsterdam and Principal Scientist at KWR Nieuwegein Other members Prof. Dr A.H. Weerts, Wageningen University & Research Dr G. van Wirdum Dr K.T. Rebel, Utrecht University Dr R.P. Bartholomeus, KWR Water, Nieuwegein This research was conducted under the auspices of the Research School for Socio- Economic and Natural Sciences of the Environment (SENSE) Hydrological controls on salinity exposure and the effects on plants in lowland polders Sija F. Stofberg Thesis submitted in fulfilment of the requirements for the degree of doctor at Wageningen University by the authority of the Rector Magnificus Prof. Dr A.P.J. Mol in the presence of the Thesis Committee appointed by the Academic Board to be defended in public on Wednesday 07 June 2017 at 4 p.m. in the Aula. Sija F. Stofberg Hydrological controls on salinity exposure and the effects on plants in lowland polders, 172 pages. PhD thesis, Wageningen University, Wageningen, the Netherlands (2017) With references, with summary in English ISBN: 978-94-6343-187-3 DOI: 10.18174/413397 Table of contents Chapter 1 General introduction .......................................................................................... 7 Chapter 2 Fresh water lens persistence and root zone salinization hazard under temperate climate ............................................................................................ 17 Chapter 3 Effects of root mat buoyancy and heterogeneity on floating fen hydrology .. -
A Study on Water and Salt Transport, and Balance Analysis in Sand Dune–Wasteland–Lake Systems of Hetao Oases, Upper Reaches of the Yellow River Basin
water Article A Study on Water and Salt Transport, and Balance Analysis in Sand Dune–Wasteland–Lake Systems of Hetao Oases, Upper Reaches of the Yellow River Basin Guoshuai Wang 1,2, Haibin Shi 1,2,*, Xianyue Li 1,2, Jianwen Yan 1,2, Qingfeng Miao 1,2, Zhen Li 1,2 and Takeo Akae 3 1 College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot 010018, China; [email protected] (G.W.); [email protected] (X.L.); [email protected] (J.Y.); [email protected] (Q.M.); [email protected] (Z.L.) 2 High Efficiency Water-saving Technology and Equipment and Soil Water Environment Engineering Research Center of Inner Mongolia Autonomous Region, Hohhot 010018, China 3 Faculty of Environmental Science and Technology, Okayama University, Okayama 700-8530, Japan; [email protected] * Correspondence: [email protected]; Tel.: +86-13500613853 or +86-04714300177 Received: 1 November 2020; Accepted: 4 December 2020; Published: 9 December 2020 Abstract: Desert oases are important parts of maintaining ecohydrology. However, irrigation water diverted from the Yellow River carries a large amount of salt into the desert oases in the Hetao plain. It is of the utmost importance to determine the characteristics of water and salt transport. Research was carried out in the Hetao plain of Inner Mongolia. Three methods, i.e., water-table fluctuation (WTF), soil hydrodynamics, and solute dynamics, were combined to build a water and salt balance model to reveal the relationship of water and salt transport in sand dune–wasteland–lake systems. Results showed that groundwater level had a typical seasonal-fluctuation pattern, and the groundwater transport direction in the sand dune–wasteland–lake system changed during different periods. -
School Level Educational Landscape with Respect to Poverty in Some Coastal Blocks of South 24 Parganas District: a Synoptic View
Pramana Research Journal ISSN NO: 2249-2976 School Level Educational Landscape with respect to Poverty in some Coastal Blocks of South 24 Parganas District: A Synoptic View Satyajit Dharaa & Kaustuv Bhattacharyyab1* a. Assistant Professor of A.J.C. Bose College, Kolkata – 20. E-mail : [email protected] b. Assistant Professor, The West Bengal University of Teachers’ Training, Education Planning and Administration [i.e.,erstwhile David Hare Training College],Kolkata – 19. E-mail : [email protected] Abstract Poverty is one of the most important socioeconomic problems in developing and less developed countries. It hinders the progress of a nation. Poverty erodes economic and social rights such as the right to health, adequate housing, food, safe drinking water and right to education. Due to globalisation the demand of higher education is increasing day by day. But for the quantitative and qualitative development of education it requires huge expenditure in the educational field. In such a circumstance - poverty is one of the most vivid problems for the spread of education in poor socioeconomic regions of a country. Better educational infrastructure can support better educational opportunities for the students. The South 24 Parganas district is situated to the extreme southern part of West Bengal. At present there are 29 blocks in this district. The southern part of the district is under the Indian Sundarban region, adjacent to the Bay of Bengal. The coastal blocks of South 24 Parganas district are Basanti-I, Canning-I&II, Gosaba, Jaynagar-I&II, Kakdwip, Sagar, Namkhana, Patharpratima, Kultali, Mathurapur-I&II. The people living here are facing high poverty and natural calamities. -
Modelling Groundwater Recharge
Groundwater recharge in Slovenia Energie & Umwelt Energie Results of a bilateral German-Slovenian Research project Energy & Environment Energy Mišo Andjelov, Zlatko Mikulič, Björn Tetzlaff, Jože Uhan & Frank Wendland 339 Groundwater recharge in Slovenia recharge Groundwater Member of the Helmholtz Association Member of the M. Andjelov, Z. Mikulič, B. Tetzlaff, J. Uhan & F. Wendland F. J. Uhan & B. Tetzlaff, Z. Mikulič, M. Andjelov, Energie & Umwelt / Energie & Umwelt / Energy & Environment Energy & Environment Band/ Volume 339 Band/ Volume 339 ISBN 978-3-95806-177-4 ISBN 978-3-95806-177-4 Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment Band / Volume 339 Forschungszentrum Jülich GmbH Institute of Bio- and Geosciences Agrosphere (IBG-3) Groundwater recharge in Slovenia Results of a bilateral German-Slovenian Research project Mišo Andjelov, Zlatko Mikulič, Björn Tetzlaff, Jože Uhan & Frank Wendland Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment Band / Volume 339 ISSN 1866-1793 ISBN 978-3-95806-177-4 Bibliographic information published by the Deutsche Nationalbibliothek. The Deutsche Nationalbibliothek lists this publication in the Deutsche Nationalbibliografie; detailed bibliographic data are available in the Internet at http://dnb.d-nb.de. Publisher and Forschungszentrum Jülich GmbH Distributor: Zentralbibliothek 52425 Jülich Tel: +49 2461 61-5368 Fax: +49 2461 61-6103 Email: [email protected] www.fz-juelich.de/zb Cover Design: Grafische Medien, Forschungszentrum Jülich GmbH Printer: Grafische Medien, Forschungszentrum Jülich GmbH Copyright: Forschungszentrum Jülich 2016 Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment, Band / Volume 339 ISSN 1866-1793 ISBN 978-3-95806-177-4 The complete volume is freely available on the Internet on the Jülicher Open Access Server (JuSER) at www.fz-juelich.de/zb/openaccess. -
Policy Options for Dryland Salinity Management: an Agent-Based Model for Catchment Level Analysis
Policy Options for Dryland Salinity Management: An Agent-Based Model for Catchment Level Analysis Keywords: Technology adoption, landholder heterogeneity, interdependencies, policy analysis, agent-based model, spatial model Shamsuzzaman Bhuiyan School of Agricultural and Resource Economics University of Western Australia CRAWLEY WA 6009 AUSTRALIA Tel: +61 8 6488 2536 Fax: +61 8 6488 1098 Abstract Dryland salinity management requires the integration of hydrologic, economic, social and policy aspects into an interactive method that decision makers can use to evaluate the economic and environmental consequences of alternative land use/management practices as well as various policy choices. This requires that modelling frameworks be open and accessible to a range of disciplines as well as allowing flexibility in exploration in learning or adapting. This interactive method will present the development of a new integrated hydrologic-economic model in the context of a catchment in which land use change is the dominant factor and salinity emergence due to land use and land cover change presents a major land and water degradation problem. This model will reflect the interactions between biophysical processes and socioeconomic processes as well as to explore both economic and environmental consequences of different policy options. All model components will be incorporated into a single consistent model, which will be solved in its entirety by an agent based modelling (ABM) approach. Agent-based Modelling (ABM) will allow to incorporate features that are necessary for a realistic representation of economic behaviour and interactions among resource managers. 1 Introduction Dryland salinity, a consequence of land use and cover changes (LUCC) is a growing problem in Australia because of threat to agriculture through the loss of productive land; to roads, houses and infrastructure through salt damage; to drinking water through increasing salt levels; and to biodiversity through the loss of native vegetation and salinisation of wetland areas (WASI 2003). -
Integrated Surface-Subsurface Water Flow Modelling of the Laxemar Area Application of the Hydrological Model ECOFLOW
R-07-07 Integrated surface-subsurface water flow modelling of the Laxemar area Application of the hydrological model ECOFLOW Nikolay Sokrut, Kent Werner, Johan Holmén Golder Associates AB January 2007 Svensk Kärnbränslehantering AB Swedish Nuclear Fuel and Waste Management Co Box 5864 SE-102 40 Stockholm Sweden Tel 08-459 84 00 +46 8 459 84 00 Fax 08-661 57 19 +46 8 661 57 19 CM Gruppen AB, Bromma, 2007 ISSN 1402-3091 Tänd ett lager: SKB Rapport R-07-07 P, R eller TR. Integrated surface-subsurface water flow modelling of the Laxemar area Application of the hydrological model ECOFLOW Nikolay Sokrut, Kent Werner, Johan Holmén Golder Associates AB January 2007 This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the authors and do not necessarily coincide with those of the client. A pdf version of this document can be downloaded from www.skb.se Abstract Since 2002, the Swedish Nuclear Fuel and Waste Management Co (SKB) performs site investigations in the Simpevarp area, for the siting of a deep geological repository for spent nuclear fuel. The site descriptive modelling includes conceptual and quantitative modelling of surface-subsurface water interactions, which are key inputs to safety assessment and environmental impact assessment. Such modelling is important also for planning of continued site investigations. In this report, the distributed hydrological model ECOFLOW is applied to the Laxemar subarea to test the ability of the model to simulate surface water and near-surface groundwater flow, and to illustrate ECOFLOW’s advantages and drawbacks. -
Government of West Bengal Office of the District
District Disaster Management Plan, South 24 Parganas 2015 Government of West Bengal Office of the District Magistrate, South 24 Parganas District Disaster Management Department New Treasury Building, (1 st Floor) Alipore, Kolkata-27 . An ISO 9001:2008 Certified Organisation : [email protected] , : 033-2439-9247 1 District Disaster Management Plan, South 24 Parganas 2015 Government of West Bengal Office of the District Magistrate, South 24-Parganas District Disaster Management Department Alipore, Kolkata- 700 027 An ISO 9001:2008 Certified Organisation : [email protected] , : 033-2439-9247 2 District Disaster Management Plan, South 24 Parganas 2015 3 District Disaster Management Plan, South 24 Parganas 2015 ~:CONTENTS:~ Chapter Particulars Page No. Preface~ 5 : Acknowledgement 6 Maps : Chapter-1 i) Administrative Map 8 ii) Climates & Water Bodies 9 Maps : iii) Roads & Railways 10 iv) Occupational Pattern 11 ~ v) Natural Hazard Map 12 District Disaster Management Committee 13 List of important phone nos. along with District Control 15 Room Number Contact number of Block Development Officer 16 Contact Details of Municipality, South 24 Parganas 17 Contact number of OC Disaster Management & 18 Chapter-2: SDDMO/BDMO Other important contact number 19 Contact details State Level Disaster Management Contact Number 26 Contact Details of Police, South 24 Parganas 29 Contact Details of PHE , PWD & I & W 35 Contact details of ADF (Marine), Diamond Harbour 37 List of Block wise GR Dealers with their contact details, 38 South 24 Parganas The Land & the River 43 Demography 49 Chapter-3: Multi Hazard Disaster Management Plan 57 District Profile History of Disaster, South 24 Parganas 59 Different types of Natural Calamities with Dos & don’ts 60 Disaster Management Plan of District Controller (F&S) 71 Chapter: 4 Disaster Disaster Management Plan of Health 74 Disaster Management Plan of WB Fire & Emergency Management Plan 81 of Various Services. -
Ground Water Information Booklet South 24 Parganas District, West Bengal
GROUND WATER INFORMATION BOOKLET SOUTH 24 PARGANAS DISTRICT, WEST BENGAL DISTRICT AT A GLANCE Sl. Items Statistics No. 1. GENERAL INFORMATION i) Geographical Area (Sq.km.) 9960 ii) Administrative Division (as on 2001) • No. of Subdivision 5 nos. • No. of Blocks 29 nos. • No. of Panchayat Samities 29 nos. • No. of Municipalities 7 nos. • No. of Gram Panchayats 312 nos. • No. of inhabited villages 4324 nos. iii) Population (as on 2001 Census) 69,06,689 iv) Normal Annual Rainfall 1800 mm 2. GEOMORPHOLOGY i) Major Physiographic Unit The deltaic plains; the levees; the marshes; and the islands of Sundarbans.. ii) Major Drainages a) Natural Hugli Matla, Bidyadhari, Raimangal, Thakuran, Saptamukhi etc. b) Artificial Bhangar khal, Kulpi khal, Surjapur khal etc. 3. LAND USE (As on 2044-05) i) Forest Area 4,263 sq.km ii) Net Area Sown 3782.7 sq.km. 4. MAJOR SOIL TYPES (i) Entisols; (ii) Alfisols; & (iii) Aridisols. 5. AREA UNDER PRINCIPAL CROPS (As on 2004-05) i) Food Grains (Rice, Wheat, 4100 sq.km. Pulses etc) ii) Oil Seeds (Rape, mustard etc.) 81 sq.km. iii) Fibres (Jute Etc.) 16 sq.km. iv) Miscellaneous crops (Potato, 49 sq.km. sugarcane etc,) 6. IRRIGATION BY DIFFERENT SOURCES i) Shallow Tubewells 136.313 sq.km. area was actually irrigated through 9278 nos. of STW during 2000-01, whereas the culturable command area (CCA) 1 through the exiting 9452 nos. of STW was 151.877 sq.km. ii) Deep Tubewells 3.434 sq.km area was actually irrigated through 28 nos. of DTW during 2000-01, whereas, the CCA through the existing 29 DTW was 7.10 sq.km.