Ocean, Atmosphere, and Climate, Lesson 7
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Kaiapoi Street Map
Kaiapoi Street Map www.northcanterbury.co.nz www.visitwaimakariri.co.nz 5 19 To Woodend, Kaikoura and Picton North To Rangiora T S S M A I L L I W 2 D R E 62 D I S M A C 29 54 E V A 64 E To Pines, O H and Kairaki 52 U T 39 45 4 57 44 10 7 63 46 47 30 8 32 59 9 38 33 24 65 11 37 66 48 18 16 23 61 26 20 17 27 25 49 13 58 14 12 28 21 51 15 22 31 41 56 50 55 3 1 35 Sponsored by 36 JIM BRYDEN RESERVE LICENSED AGENT REAA 2008 To Christchurch Harcourts Twiss-Keir Realty Ltd. 6 MREINZ Licensed Agent REAA 2008. Phone: 03 327 5379 Email: [email protected] Web: www.twisskeir.co.nz 40 60 © Copyright Enterprise North Canterbury 2016 For information and bookings contact Kaiapoi i-SITE Visitor Centre Kaiapoi Street and Information Index Phone 03 327 3134 Adams Street C5 Cressy Ave F3 Lees Rd A5 Sneyd St F2 Accommodation Attractions Adderley Tce E2 Cridland St E4 Lower Camside Rd B4 Sovereign Bvd C5 1 H3 Blue Skies Holiday & Conference Park 32 F4 Kaiapoi Historic Railway Station Akaroa St G3 Cumberland Pl H2 Magnate Dr C5 Stark Pl D5 2 C4 Grenmora B & B 55 Old North Rd 33 F4 Kaiapoi Museum And Art Gallery Aldersgate St G2 Dale St D4 Magnolia Bvd D5 Sterling Cres C5 3 H3 Kaiapoi on Williams Motel 35 H3 National Scout Museum Alexander Ln F3 Davie St F4 Main Drain Rd D1 Stone St H4 64 F6 Kairaki Beach Cottage 36 H5 Woodford Glen Speedway Allison Cres D5 Dawson Douglas Pl G4 Main North Rd I3 Storer St F1 4 F3 Morichele B & B Alpine Ln F3 Day Pl F5 Mansfield Dr G3 Sutherland Dr C6 5 A5 Pine Acres Holiday Park & Motels Recreation Ansel Pl D5 Doubledays -
Rain Shadows
WEB TUTORIAL 24.2 Rain Shadows Text Sections Section 24.4 Earth's Physical Environment, p. 428 Introduction Atmospheric circulation patterns strongly influence the Earth's climate. Although there are distinct global patterns, local variations can be explained by factors such as the presence of absence of mountain ranges. In this tutorial we will examine the effects on climate of a mountain range like the Andes of South America. Learning Objectives • Understand the effects that topography can have on climate. • Know what a rain shadow is. Narration Rain Shadows Why might the communities at a certain latitude in South America differ from those at a similar latitude in Africa? For example, how does the distribution of deserts on the western side of South America differ from the distribution seen in Africa? What might account for this difference? Unlike the deserts of Africa, the Atacama Desert in Chile is a result of topography. The Andes mountain chain extends the length of South America and has a pro- nounced influence on climate, disrupting the tidy latitudinal patterns that we see in Africa. Let's look at the effects on climate of a mountain range like the Andes. The prevailing winds—which, in the Andes, come from the southeast—reach the foot of the mountains carrying warm, moist air. As the air mass moves up the wind- ward side of the range, it expands because of the reduced pressure of the column of air above it. The rising air mass cools and can no longer hold as much water vapor. The water vapor condenses into clouds and results in precipitation in the form of rain and snow, which fall on the windward slope. -
REFEREES the Following Are Amongst Those Who Have Acted As Referees During the Production of Volumes 1 to 25 of the New Zealand Journal of Forestry Science
105 REFEREES The following are amongst those who have acted as referees during the production of Volumes 1 to 25 of the New Zealand Journal of Forestry Science. Unfortunately, there are no records listing those who assisted with the first few volumes. Aber, J. (University of Wisconsin, Madison) AboEl-Nil, M. (King Feisal University, Saudi Arabia) Adams, J.A. (Lincoln University, Canterbury) Adams, M. (University of Melbourne, Victoria) Agren, G. (Swedish University of Agricultural Science, Uppsala) Aitken-Christie, J. (NZ FRI, Rotorua) Allbrook, R. (University of Waikato, Hamilton) Allen, J.D. (University of Canterbury, Christchurch) Allen, R. (NZ FRI, Christchurch) Allison, B.J. (Tokoroa) Allison, R.W. (NZ FRI, Rotorua) Alma, P.J. (NZ FRI, Rotorua) Amerson, H.V. (North Carolina State University, Raleigh) Anderson, J.A. (NZ FRI, Rotorua) Andrew, LA. (NZ FRI, Rotorua) Andrew, LA. (Telstra, Brisbane) Armitage, I. (NZ Forest Service) Attiwill, P.M. (University of Melbourne, Victoria) Bachelor, C.L. (NZ FRI, Christchurch) Bacon, G. (Queensland Dept of Forestry, Brisbane) Bagnall, R. (NZ Forest Service, Nelson) Bain, J. (NZ FRI, Rotorua) Baker, T.G. (University of Melbourne, Victoria) Ball, P.R. (Palmerston North) Ballard, R. (NZ FRI, Rotorua) Bannister, M.H. (NZ FRI, Rotorua) Baradat, Ph. (Bordeaux) Barr, C. (Ministry of Forestry, Rotorua) Bartram, D, (Ministry of Forestry, Kaikohe) Bassett, C. (Ngaio, Wellington) Bassett, C. (NZ FRI, Rotorua) Bathgate, J.L. (Ministry of Forestry, Rotorua) Bathgate, J.L. (NZ Forest Service, Wellington) Baxter, R. (Sittingbourne Research Centre, Kent) Beath, T. (ANM Ltd, Tumut) Beauregard, R. (NZ FRI, Rotorua) New Zealand Journal of Forestry Science 28(1): 105-119 (1998) 106 New Zealand Journal of Forestry Science 28(1) Beekhuis, J. -
Hurricane Paths: Comparing Places with Different Prevailing Winds
Name ___________________________ Hurricane Paths: Comparing Places with Different Prevailing Winds To understand where hurricanes usually start and what direction they usually move, it helps to have a clear mental image of the pattern of prevailing winds in the world. One way to get this image is to make a careful comparison of wind observations in several places. The diagrams on the right are examples of a special kind of graph called a wind rose. The number in the center indicates the percentage of time the air is calm (no wind). Each of the eight lines radiating away from the center shows the percentage of time the wind blows FROM that direction. Repeat: The lines point to the direction the wind is blowing FROM. Please answer the following questions. 1) According to the map above, Boston has calm air about 12% of the time; the percentage of time San Juan, Puerto Rico, has calm air is _____ . 2) In San Juan, the wind blows the largest percentage of time from the northeast; in Boston, the wind blows from the _________ more often than from any other direction. 3) Use the wind rose graphs on pages 2 and 3. To get an idea about the net zonal flow of air in each location, add up the total percentage of time the wind blows from the southwest, west, and northwest, and subtract the total percentage from the southeast, east, and northeast total percentage. The result is the net westerly component - it is a positive number if the flow is mainly westerly (from the west), and a negative number if the flow is easterly (from the east). -
Investment Prospectus Interconnected | Cutting Edge | World Class
DUNEDIN, NEW ZEALAND INVESTMENT PROSPECTUS Interconnected | Cutting Edge | World Class BUSINESS We consider ourselves very fortunate ARCHITECTURE to be able to easily tap into a wealth of design talent and advice from the Otago Polytechnic that’s really boosted our VAN BRANDENBERG global project. Damien van Brandenberg Architecture Van Brandenberg CONTENTS Dunedin, New Zealand, The Business Centre of the South 03 Dunedin Investment Opportunities 05 Vital Statistics 06 Education and Learning 11 Case Study: Lauguage Perfect 12 Human and Animal Health – Health Technologies 15 Case Study: Pacific Edge Ltd 16 Design Technology and Niche Manufacturing 18 Case Study: Escea 20 Access to Markets 22 Resources – People, Support, Research and Land 24 Investor Returns for Property in Dunedin 26 The Regulatory Environment 29 Business Culture and Lifestyle 30 Further Information, Useful Links and Data Sources 36 The authors have made every effort to ensure that the information contained in this publication is reliable but they make no guarantee of its accuracy and completeness and do not accept liability for any errors. Information may change at any time. The information in this prospectus is of a general nature and should be used as a guide only. The companies referred to in this publication are not an exhaustive list and do not comprise all companies located in the city. 01 As a European migrant moving my family of eight to Dunedin from Germany, I am reassured by the friendliness, practical help and optimism that I have found here. Clearly there are business opportunities to create and build on and a thriving business network. -
Submission on Selwyn District Council Draft Long Term Plan 2018-2028
Submission on Selwyn District Council Draft Long Term Plan 2018-2028 To: Selwyn District Council Submitter: Community & Public Health A division of the Canterbury District Health Board Attn: Kirsty Peel Community and Public Health C/- Canterbury District Health Board PO Box 1475 Christchurch 8140 Proposal: Selwyn District Council is consulting on their long-term plan to ascertain views on how best to manage infrastructure and services in the district over the next 10 years. Page 1 of 9 Template File Pathway: Y:\CFS\CPHGroups\RMC\SDC\LTP\2018\SelwynLTPSubmissionFinal180503.docx SUBMISSION ON SELWYN DISTRICT COUNCIL DRAFT LONG TERM PLAN Details of submitter 1. Canterbury District Health Board (CDHB) 2. The CDHB is responsible for promoting the reduction of adverse environmental effects on the health of people and communities and to improve, promote and protect their health pursuant to the New Zealand Public Health and Disability Act 2000 and the Health Act 1956. 3. These statutory obligations are the responsibility of the Ministry of Health and, in the Canterbury District, are carried out under contract by Community and Public Health under Crown funding agreements on behalf of the Canterbury District Health Board. General comments 4. Health and wellbeing (overall quality of life) is influenced by a wide range of factors beyond the health sector. These influences can be described as the conditions in which people are born, grow, live, work and age, and are impacted by environmental, social and behavioural factors. They are often referred to as the ‘social determinants of health1. Barton and Grant’s Health Map2 shows how various influences on health are complex and interlinked. -
Comparison of Liquefaction-Induced Land Damage and Geomorphic Variability in Avonside, New Zealand
6th International Conference on Earthquake Geotechnical Engineering 1-4 November 2015 Christchurch, New Zealand Comparison of Liquefaction-induced Land Damage and Geomorphic Variability in Avonside, New Zealand S.H. Bastin1, M.C. Quigley2, K. Bassett3 Abstract Field mapping, LiDAR, and aerial photography are used to map surface liquefaction-induced lateral spreading fissures and aligned sand blow vents formed during the 22 February 2011 Mw 6.2 Christchurch earthquake. Classification of the study area into 164 polygons enables comparison of liquefaction severity metrics including linear liquefaction feature density, ejecta surface area, and horizontal and vertical ground surface displacements with geomorphic metrics including distance from the downslope free-face, surface elevation, sediment type, and the liquefaction potential index (LPI). Preliminary analyses indicate (i) mean fissure density decreases with increasing distance from the free face at distances of 0-50 m, no relationship is observed at distances >50 m, (ii) mean horizontal ground displacement increases with increasing LPI, and (iii) vertical subsidence is invariant with elevation, implying that other factors (e.g. LPI) may contribute to a complex liquefaction strain field. The basic geology and geomorphology are derived from LiDAR and modern river morphology. Comparison of the liquefaction data with geomorphic mapping indicates geomorphic mapping may be applied to determine the likely distribution of sediments susceptible to liquefaction. Introduction Cyclic shearing of loosely consolidated, fluid saturated sediments during earthquake-induced ground motion results in excess pore-water pressures and reduced shear strength in the affected media. Liquefaction occurs as the grain arrangement collapses causing pore water pressures to exceed the confining pressure (Seed & Idriss, 1982; Idriss & Boulanger, 2008). -
Winter-Hawaii/Australia)
CELEBRITY ECLIPSE® — SEPTEMBER 2022 - APRIL 2023 (WINTER-HAWAII/AUSTRALIA) Date Nights Description Ports British Columbia: Vancouver, At Sea, At Sea, At Sea, At Sea, At Sea, Hawaii: Hilo, Hawaii: Kailua Kona, Hawaii: Lahaina, Maui (overnight), 22-Sept-22 11 Hawaii Kilauea Volcano, Hawaii: Honolulu, Oahu Hawaii: Honolulu, Oahu, At Sea, At Sea, At Sea, At Sea, At Sea, French Polynesia: Papeete, Tahiti, French Polynesia: Bora Bora, French Hawaii, Tahiti, 3-Oct-22 18 Polynesia: Moorea, At Sea, At Sea, International Date Line, At Sea, At Sea, At Sea, At Sea, New Zealand: Auckland, New Zealand: Bay of & Bora Bora Islands, At Sea, At Sea, Australia: Sydney 22-Oct-22 Australia: Sydney, At Sea, At Sea, New Zealand: Milford Sound, New Zealand: Doubtful Sound, New Zealand: Dusky Sound, New Zealand: 27-Nov-22 12 New Zealand Dunedin, New Zealand: Christchurch, New Zealand: Wellington, New Zealand: Napier, New Zealand: Tauranga, New Zealand: Auckland, 16-Feb-23 At Sea, At Sea, Australia: Sydney Australia: Sydney, At Sea, Australia: Brisbane, At Sea, Australia: Wills Island (Cruising), Australia: Port Douglas, Australia: Cairns (Yorkey’s 3-Nov-22 11 Great Barrier Reef Knob), Australia: Airlie Beach, Queensland, At Sea, At Sea, Australia: Sydney (overnight) Australia: Sydney, At Sea, At Sea, New Zealand: Milford Sound, New Zealand: Doubtful Sound, New Zealand: Dusky Sound, New 14-Nov-22 13 New Zealand Zealand: Dunedin, New Zealand: Christchurch, New Zealand: Picton, New Zealand: Napier, New Zealand: Tauranga, New Zealand: Auckland, New Zealand: Bay of -
Prevailing Wind Park Energy Facility Draft Environmental Assessment
Prevailing Wind Park Energy Facility Draft Environmental Assessment DOE/EA-2061 January 2019 Prevailing Wind Park Energy Facility Draft Environmental Assessment Bon Homme, Charles Mix, Hutchinson, and Yankton Counties, South Dakota U.S. Department of Energy Western Area Power Administration DOE/EA-2061 January 2019 Prevailing Wind Park Draft EA Table of Contents TABLE OF CONTENTS Page No. 1.0 INTRODUCTION ............................................................................................... 1-1 1.1 WAPA’s Purpose and Need ................................................................................. 1-3 1.2 Prevailing Wind Park’s Goals and Objectives ..................................................... 1-3 2.0 DESCRIPTION OF PROPOSED ACTION AND NO ACTION ALTERNATIVES ............................................................................................... 2-1 2.1 Proposed Action ................................................................................................... 2-1 2.1.1 Prevailing Wind Park Project ................................................................ 2-1 2.1.2 Project Life Cycle ................................................................................. 2-5 2.2 No Action Alternative .......................................................................................... 2-5 3.0 AFFECTED ENVIRONMENT ............................................................................ 3-1 3.1 Land Cover and Land Use .................................................................................. -
FINAL REPORT Wind Assessment For: BANKSTOWN
FINAL REPORT Wind Assessment for: BANKSTOWN COMPASS CENTRE 83-99 North Terrace & 62 The Mall, Bankstown Sydney, NSW 2200, Australia Prepared for: Fioson Pty Ltd L34, 225 George St Sydney NSW 2000 CPP Project: 8759 October 2016 Prepared by: Thomas Evans, Engineer Graeme Wood, Ph.D., Director CPP Project 8759 Executive Summary This report provides an opinion based qualitative assessment of the impact of the proposed Bankstown Compass Centre development on the local pedestrian-level wind environment. This assessment is based on knowledge of the local Bankstown wind climate and previous wind- tunnel test on similar buildings in the Bankstown area. The proposed development is taller than surrounding buildings. Wind speeds are expected to be higher around the outer corners of the development, though the podium roof will prevent significant wind effects occurring at street level. The environmental wind conditions at ground level around the proposed development are expected to be suitable for pedestrian standing from a comfort perspective and pass the distress criterion. Within the development, wind conditions are expected to be suitable for pedestrian standing or walking activities and pass the distress criterion under Lawson. For such a large development with several similar sized towers designed in such a complex manner, it would be recommended to quantify the wind conditions and confirm the qualitative findings using wind-tunnel testing. ii CPP Project 8759 DOCUMENT VERIFICATION Prepared Checked Approved Date Revision by by by 04/02/16 Final Report KF GSW GSW 10/02/16 Revision 1 KF GSW GSW 04/10/16 Amended design drawings TE GSW GSW 05/10/16 Amended Figure TE GSW GSW TABLE OF CONTENTS Executive Summary ............................................................................................................................... -
Points Statement
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T5.1 the Dynamics of Nova Scotia's Climate
PAGE .............................................................. 94 ▼ T5.1 THE DYNAMICS OF NOVA SCOTIA’S CLIMATE The main features of Nova Scotia’s climate are am- MAJOR AIR MASSES ple and reliable precipitation, a fairly wide but not extreme temperature range, a late and short sum- Satellite photography, computer modelling, a greater mer, skies that are often cloudy or overcast, frequent knowledge of the structure of weather systems and a coastal fog and marked changeability of weather better understanding of the physical processes that from day to day. These features can be related to four control our weather have all led to a much-reduced basic factors: use of air-mass concepts. Air-mass theory is still 1. the prevailing westerly winds used descriptively, however, and is very useful to 2. the interactions between the three main air introduce people to the disciplines of meteorology masses which converge on the east coast and climatology. 3. Nova Scotia’s position astride the routes of the Much of the variability of the weather is caused by major eastward-moving storms the shifting positions of the three main air masses T5.1 4. the modifying influence of the sea that dominate the eastern seaboard. Continental The Dynamics of arctic air from the northwest is very dry and cold in Nova Scotia’s WIND SYSTEMS winter. Maritime polar air, moving in from the north Climate or northeast, has been somewhat warmed by its The basic eastward movement of the wind systems passage over the ocean and is cool and moist. Mari- (known as the westerlies) over North America is a time tropical air from the south or southwest is warm result of the general circulation of warm air from the and moist.