Air-Sea Flux Measurements Over the Southern Ocean

Total Page:16

File Type:pdf, Size:1020Kb

Air-Sea Flux Measurements Over the Southern Ocean Air-Sea Flux Measurements over the Southern Ocean David James Tupman Submitted in accordance with the requirements for the degree of Doctor of Philosophy The University of Leeds School of Earth and Environment August 2013 The candidate confirms that the work submitted is his own and that appropriate credit has been given where reference has been made to the work of others. This copy has been supplied on the understanding that it is copyright material and that no quotation from the thesis may be published without proper acknowledgement. - 1 - Acknowledgements I would primarily like to thank Ian Brooks for supervision, guidance, and comments throughout the period of study, and the rest of the air-sea interaction group at ICAS. Thanks to all at NOC and BAS who contributed to the WAGES project, but particularly to Margaret Yelland and John Prytherch for many useful discussions and comments. Many thanks of course to all at ICAS who made my time at Leeds and working life there so enjoyable. - 2 - Abstract The Waves, Aerosol, and Gas Exchange Study (WAGES) collected 18 months of near-continuous and autonomous turbulent air-sea flux estimates from the research vessel RRS James Clark Ross. Supporting meteorological and sea-state measurements were also made, with the objective of improving air-sea flux parameterisations. Making turbulence measurements from a ship is technically challenging, due to bias caused by platform motion and airflow distortion. Typically, visual inspection of individual turbulence spectra is needed to quality control eddy covariance flux estimates; for WAGES the sheer volume of data motivated the development of an automated quality control method, to be performed on individual flux cospectra. The application of these tests allowed a robust relationship between the 10 m wind speed and the neutral drag coefficient to be developed, which had previously not been achieved with ship-based covariance measurements alone. This parameterisation is toward the higher end of the range of accepted values, and indicates some wind speed dependence of the Charnock parameter, rather than it being a constant. A detailed investigation of turbulent flow distortion was made; insights into the physics were gained, and a novel correction method for motion-correlated flow distortion was developed and validated. Two major modes of motion-correlated flow distortion of the turbulence were found: one correlated to the pitch, acknowledge in the literature; a second and more powerful mode correlated to the rate of change of the pitch, not acknowledged in any publication. The quality control and bias correction techniques developed for the momentum fluxes were transferred to a preliminary investigation of the sensible and latent heat fluxes. The uncertainty in the latent heat transfer coefficient was reduced considerably by use of the new techniques; however the sensible heat fluxes were dominated by noise, so discarded. The methods and corrections developed in this thesis could be used to re- analyse the turbulent flux measurements from many ship-based campaigns; improving our understanding of the physics of air-sea exchange without need for additional expensive measurements. - 3 - Contents Acknowledgements ...............................................................................................- 2 - Abstract..................................................................................................................- 3 - Contents .................................................................................................................- 4 - Figures....................................................................................................................- 7 - Tables ...................................................................................................................- 12 - 1 Introduction................................................................................................- 13 - 2 Literature Review ......................................................................................- 18 - 2.1 The atmospheric surface layer above an infinite flat surface............................... - 18 - 2.1.1 Qualitative description of the surface layer .................................................. - 18 - 2.1.2 Quantitative surface layer relationships........................................................ - 22 - 2.1.3 Turbulence Spectra ....................................................................................... - 27 - 2.2 Wave influences on the surface layer................................................................... - 31 - 2.2.1 Stress and turbulent spectra .......................................................................... - 34 - 2.2.2 Vertical wind profile..................................................................................... - 40 - 2.2.3 Effects on TKE terms.................................................................................... - 42 - 2.3 Airflow distortion................................................................................................. - 43 - 2.4 Flux parameterisations ......................................................................................... - 45 - 2.4.1 Wind speed dependence................................................................................ - 45 - 2.4.2 Sea State influence........................................................................................ - 51 - 2.5 Literature review summary .................................................................................. - 54 - 3 WAGES.......................................................................................................- 55 - 3.1 Overview .............................................................................................................. - 55 - 3.1.1 Transition from HiWASE to WAGES.......................................................... - 55 - 3.2 Instrumentation..................................................................................................... - 57 - 3.2.1 Flux instrumentation ..................................................................................... - 57 - 3.2.2 Meteorology and sea state sensors................................................................ - 61 - 3.2.3 Data Logging ................................................................................................ - 63 - 3.3 Post-cruise processing.......................................................................................... - 64 - 3.3.1 Conversion into Matlab compatible files...................................................... - 65 - 3.3.2 Spike removal ............................................................................................... - 66 - - 4 - 3.3.3 Synchronisation of flux sensors.................................................................... - 67 - 3.3.4 Motion Correction......................................................................................... - 68 - 3.3.5 Rotation into the streamline frame of reference ........................................... - 74 - 3.3.6 Choice of time series length.......................................................................... - 77 - 3.3.7 Mean temperature and relative humidity ...................................................... - 79 - 3.3.8 Calculation of mean conditions .................................................................... - 82 - 3.3.9 Calculation of fluxes..................................................................................... - 85 - 3.4 Quality control...................................................................................................... - 86 - 3.4.1 Major events and data losses......................................................................... - 86 - 3.5 Flux Results.......................................................................................................... - 95 - 3.6 Summary ............................................................................................................ - 102 - 4 Automated spectral quality control........................................................- 104 - 4.1 Common contamination types............................................................................ - 105 - 4.2 Overview ............................................................................................................ - 108 - 4.3 Kaimal form fitting............................................................................................. - 110 - 4.4 Motion contamination ........................................................................................ - 111 - 4.4.1 Ship motion frequency band detection ....................................................... - 111 - 4.4.2 Motion contamination and interpolation..................................................... - 113 - 4.5 High frequency contamination........................................................................... - 117 - 4.6 Cospectral peak frequency rejection .................................................................. - 119 - 4.7 Relative wind direction restrictions.................................................................... - 121 - 4.8 General quality test............................................................................................. - 124 - 4.9 Results ................................................................................................................ - 126 - 4.10 Summary........................................................................................................
Recommended publications
  • Soaring Weather
    Chapter 16 SOARING WEATHER While horse racing may be the "Sport of Kings," of the craft depends on the weather and the skill soaring may be considered the "King of Sports." of the pilot. Forward thrust comes from gliding Soaring bears the relationship to flying that sailing downward relative to the air the same as thrust bears to power boating. Soaring has made notable is developed in a power-off glide by a conven­ contributions to meteorology. For example, soar­ tional aircraft. Therefore, to gain or maintain ing pilots have probed thunderstorms and moun­ altitude, the soaring pilot must rely on upward tain waves with findings that have made flying motion of the air. safer for all pilots. However, soaring is primarily To a sailplane pilot, "lift" means the rate of recreational. climb he can achieve in an up-current, while "sink" A sailplane must have auxiliary power to be­ denotes his rate of descent in a downdraft or in come airborne such as a winch, a ground tow, or neutral air. "Zero sink" means that upward cur­ a tow by a powered aircraft. Once the sailcraft is rents are just strong enough to enable him to hold airborne and the tow cable released, performance altitude but not to climb. Sailplanes are highly 171 r efficient machines; a sink rate of a mere 2 feet per second. There is no point in trying to soar until second provides an airspeed of about 40 knots, and weather conditions favor vertical speeds greater a sink rate of 6 feet per second gives an airspeed than the minimum sink rate of the aircraft.
    [Show full text]
  • Advisory Circular 91-70A
    U.S. Department Advisory of Transportation Federal Aviation Administration Circular Subject: Oceanic and International Date: 8/12/10 AC No: 91-70A Operations Initiated by: AFS-400 Change: FOREWORD This advisory circular (AC) contains general information and guidance for operators planning oceanic flights, including authorizations needed for operations outside the continental United States. This includes Special Areas of Operation (SAO) such as North Atlantic Minimum Navigation Performance Specifications (NAT/MNPS), Reduced Vertical Separation Minimum (RVSM), Area Navigation (RNAV), and Required Navigation Performance (RNP) airspace. The dynamics of oceanic operations are such that they are constantly evolving and it is incumbent on the operators to closely monitor any changes. The Federal Aviation Administration (FAA) revised this AC to point the reader to the most current sources of international material. In many cases, the references are to a Web site. The material, however, is still found at www.faa.gov or calling a Federal Aviation Administration (FAA) navigation specialist. This AC includes specific guidance for authorizations and other FAA policy issues. A detailed study of the FAA Web site is the best source for introduction information about oceanic, international, and remote operations. John M. Allen Director, Flight Standards Service AC 91-70A 8/12/10 CONTENTS Paragraph Page CHAPTER 1. GENERAL 1-1. Purpose...........................................................................................................................1
    [Show full text]
  • To Marine Meteorological Services
    WORLD METEOROLOGICAL ORGANIZATION Guide to Marine Meteorological Services Third edition PLEASE NOTE THAT THIS PUBLICATION IS GOING TO BE UPDATED BY END OF 2010. WMO-No. 471 Secretariat of the World Meteorological Organization - Geneva - Switzerland 2001 © 2001, World Meteorological Organization ISBN 92-63-13471-5 NOTE The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the World Meteorological Organization concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. TABLE FOR NOTING SUPPLEMENTS RECEIVED Supplement Dated Inserted in the publication No. by date 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 CONTENTS Page FOREWORD................................................................................................................................................. ix INTRODUCTION......................................................................................................................................... xi CHAPTER 1 — MARINE METEOROLOGICAL SERVICES ........................................................... 1-1 1.1 Introduction .................................................................................................................................... 1-1 1.2 Requirements for marine meteorological information....................................................................... 1-1 1.2.1
    [Show full text]
  • Significant Papers from the First 50 Years of the Boulder Labs
    B 0 U l 0 I R LABORATORIES u.s. Depan:ment • "'.."'c:omn-..""""....... 1954 - 2004 NISTIR 6618 and NTIA SP-04-416 Significant Papers from the First 50 Years of the Boulder Labs Edited by M.E. DeWeese M.A. Luebs H.L. McCullough u.s. Department of Commerce Boulder Laboratories NotionallnstitlJte of Standards and Technology Notional Oc::eonic and Atmospheric Mministration Notional Telecommunications and Informofion Administration NISTIR 6618 and NTIA SP-04-416 Significant Papers from the First 50 Years of the Boulder Labs Edited by M.E. DeWeese, NIST M.A. Luebs, NTIA H.L. McCullough, NOAA Sponsored by National Institute of Standards and Technology National Telecommunications and Information Administration National Oceanic and Atmospheric Administration Boulder, Colorado August 2004 U.S. Department of Commerce Donald L. Evans, Secretary National Institute of Standards and Technology Arden L. Bement, Jr., Director National Oceanic and Atmospheric Administration Conrad C. Lautenbacher, Jr., Undersecretary of Commerce for Oceans and Atmosphere and NOAA Administrator National Telecommunications and Information Administration Michael D. Gallagher, Assistant Secretary for Communications and Information ii Acronym Definitions CEL Cryogenic Engineering Laboratory CIRES Cooperative Institute for Research in Environmental Sciences CRPL Central Radio Propagation Laboratory CU University of Colorado DOC Department of Commerce EDS Environmental Data Service ERL ESSA Research Laboratory ESSA Environmental Science Services Administration ITS Institute for
    [Show full text]
  • CGMS-19 Report
    REPORT OF THE NINETEENTH MEETING OF THE CO-ORDINATION GROUP FOR METEOROLOGICAL SATELLITES CGMS XIX TASHKENT, USSR 10 - 14 DECEMBER 1990 REPORT OF THE NINETEENTH MEETING OF THE CO-ORDINATION GROUP FOR METEOROLOGICAL SATELLITES CGMS XIX TASHKENT, USSR 10 - 14 DECEMBER 1990 A. PRELIMINARIES A.1 Introduction CGMS-XIX was convened at 10.30 am on 10 December by Mr. V. Kharitonov, Deputy Director of the satellite division, Hydromet Centre of the USSR, Moscow. In his welcome address, Mr N.N. Aksarin, Director of the Uzbekistan Met Service expressed his great pleasure that CGMS had chosen Tashkent as the meeting venue for CGMS XIX. Tashkent, he added, would be one of the main data processing centres for GOMS. The construction of the building was complete and a new computer system was currently being installed. He noted that the meteorological centre in Tashkent was already very aware of the importance of satellite imagery for weather forecasting, especially for observing the weather in neighbouring rather data sparse regions. Satellite data had been received in the centre for some 20 years. He looked forward to a close cooperation with the Members of CGMS over the coming years and wished the delegates a very enjoyable stay in Tashkent and a most productive and successful The reader should note that a full list of acronyms and abbreviations can be found in Annex I. A.2 Election of Chairman Mr D.E. Hinsman, Senior Scientific Officer, Satellite Activities, WMO, was elected Chairman of this session of CGMS. Mr N.F. Veltishchev, Deputy Director of the Hydromet Centre of the USSR, Moscow, was elected Vice Chairman.
    [Show full text]
  • Planning for Delay: Influence of Flight Scheduling on Airline Punctuality
    Planning for Delay: influence of flight scheduling on airline punctuality EUROCONTROL Trends in Air Traffic Volume 7 EUROCONTROL Acknowledgements The idea for this study came from the Performance Review Commission reporting on the performance of European Air Navigation Services (ANS) in 2008 in the Performance Review Report (PRR20081). The PRR2008 reports on Key Performance Areas of Safety, Punctuality and Predictability, Capacity/delays, Flight-Efficiency, Cost- Effectiveness and Environmental impact. Within the area of punctuality and predictability, a comparison between the USA and Europe showed similar arrival punctuality rates albeit with higher variability in the US. In section 7.4.4 of PRR2008 we read that “The gap between departure and arrival punctuality is significant in the US and quasi nil in Europe”. This document has been developed to help explain why this gap is so small in Europe and how airlines themselves can influence it. Bo Redeborn, EUROCONTROL Director Cooperative Network Design, approved the further development of this series of studies with the objective of increasing the depth of knowledge. I am grateful to him for his support and encouragement. Thanks go to the STATFOR team, Claire Leleu and Magda Gregorova for their technical support and expertise. I am grateful to EUROCONTROL’s Corporate Communications Service, Caroline Cochaux and Lucia Pasquini for their help in the design and publication of this document. Thanks go to a number of people who gave their input, reviewed the document, suggested changes and helped in the proof reading. Notable amongst these were Milena Studic during her traineeship at CODA, Eric Moyson from IACA, Mark Deacon from Monarch Airlines, Daniella Massart from Brussels Airlines, Gerrit Klempert and Jens Armenat from Lufthansa.
    [Show full text]
  • UK SOLAS: Programme Final Report
    Surface Ocean-Lower Atmosphere Study UK SOLAS: Programme Final Report Authors: Phil Williamson, Chris Adams & Kay Heuser UK SOLAS Surface Ocean-Lower Atmosphere Study Programme Final Report March 2011 Phil Williamson1,2, Chris Adams1 & Kay Heuser2 1. School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ 2. Natural Environment Research Council, Polaris House, North Star Avenue, Swindon SN2 1EU Contact: [email protected] +(44)1603 59311 UK SOLAS was a NERC Research Programme, with support of £10.3m mainly over the period 2004-2010. Data management and some projects are still ongoing. Acknowledgements The authors wish to thank the UK SOLAS Scientific Steering Committee and all other UK SOLAS participants (n = >180, see p 60-63) for ensuring the success of the programme. Their contributions to this programme Final Report are much appreciated, through project final reports, cruise reports, publications and other material. Claire Hughes, Martin Johnson and Georgia Bayliss-Brown provided invaluable support for UK SOLAS science coordination in the initial and mid-phases of programme implementation, whilst the key roles of Swindon Office staff (Mike Webb, Programme Manager; Sarah Collinge, Sophie Hodgson, Frances Collingborn and Michal Filtness, Programme Administrators; and Rebecca Farncombe, finale event coordinator) are also gratefully acknowledged. Co-support of component activities was provided by the UK Meteorological Office, the European COST Action 735, the Norwegian Meteorological Office, the Cape Verde government,
    [Show full text]
  • UK SOLAS Data Management Plan 52 Includes the UK SOLAS Data Policy and Metadata Protocols
    Surface Ocean-Lower Atmosphere Study UK SOLAS: Programme Final Report Authors: Phil Williamson, Chris Adams & Kay Heuser UK SOLAS Surface Ocean-Lower Atmosphere Study Programme Final Report February 2011 Phil Williamson1,2, Chris Adams1 & Kay Heuser2 1. School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ 2. Natural Environment Research Council, Polaris House, North Star Avenue, Swindon SN2 1EU Contact: [email protected] +(44)1603 59311 UK SOLAS was a NERC Research Programme, with support of £10.3m mainly over the period 2004-2010. Data management and some projects are still ongoing. Acknowledgements The authors wish to thank the UK SOLAS Scientific Steering Committee and all other UK SOLAS participants (n = >180, see p 59-62) for ensuring the success of the programme. Their contributions to this programme Final Report are much appreciated, through project final reports, cruise reports, publications and other,material. Claire Hughes, Martin Johnson and Georgia Bayliss-Brown provided invaluable support for UK SOLAS science coordination in the initial and mid-phases of programme implementation, whilst the key roles of Swindon Office staff (Mike Webb, Programme Manager; Angela Collinge, Sophie Hodgson, Frances Collingborn and Michal Filtness, Programme Administrators; and Rebecca Farncombe, finale event coordinator) are also gratefully acknowledged. Co-support of component activities was provided by the UK Meteorological Office, the European COST Action 735, the Norwegian Meteorological Office, the Cape Verde
    [Show full text]
  • Winter Cloud Seeding Potential on the Mogollon
    WINTER CLOUD SEEDIN POTENTIAL ON THE MOGOLLON RIM FINAL REPORT PREPARED FOR ARIZONA DEPARTMENT OF WATER RESOURCES UNDER IGA-88-6189-000-0051 JANUARY 1989 , U.S. DEPARTMENT OF THE INTERIOR Bureau of Reclamation Denver Research and laboratory Services DivWon Water Augmentation Group POTENTIAL ON THE EPORTPREPAREDFOR ARIZONA DEPARTMENT OF WATER RESOURCES UNDER IGA-88-6189-000-0051 03720 7. AUTHOR(S) 8. PERFORMING ORGANIZATION REPORT NO. Arlin B. Super, Edmond W. Hdroyd, Ill, and Jack T. McPartland R-89-02 9. PERFORMING ORGANIZATION NAME AND ADDRESS 10. WORK UNIT NO. Bureau of Reclamation Denver Office 11. CONTRACT OR GRANT NO. Denver CO 80225 IGA-88-6189-000-0051 13. TYPE OF REPORT AND PERIOD - COVERED 12. SPONSORING AGENCY NAME AND ADDRESS I State of Arizona I Department of Water Resources 1 15 South 15th Avenue 14. SPONSORING AGENCY CODE R 15. SUPPLEMENTARY NOTES I Microfiche and hard copy available at the Denver Office, Denver, Colorado. 16. ABSTRACT Natural doud and precipitation processes were investigated on the Mogollon Rim of Arizona during midJanuary to midMarch of 1987 and 1988. The primary goal was to evaluate the cloud seeding potential of winter storms prior to attempting any seeding. It was crucial to monitor the availability of supercooled CLW (cloud liquid water) required for precipitation development, and this was accomplished with a ground-based microwave radiometer and instrumented aircraft. Other measurements of importance included doud depth and structure, atmospheric stabilii, winds, doud ice particles and water droplets, and surface precipitation. The field measurements were put in the context of large-scale weather patterns using standard weather maps and satellite photographs.
    [Show full text]
  • Chapter 21 100 Years of Progress in Polar Meteorology
    CHAPTER 21 WALSH ET AL. 21.1 Chapter 21 100 Years of Progress in Polar Meteorology JOHN E. WALSH International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, Alaska DAVID H. BROMWICH Byrd Polar and Climate Research Center, The Ohio State University, Columbus, Ohio JAMES.E.OVERLAND NOAA Pacific Marine Environmental Laboratory, Seattle, Washington MARK C. SERREZE National Snow and Ice Data Center, University of Colorado Boulder, Boulder, Colorado KEVIN R. WOOD Joint Institute for the Study of the Atmosphere and Oceans, University of Washington, Seattle, Washington ABSTRACT The polar regions present several unique challenges to meteorology, including remoteness and a harsh en- vironment. We summarize the evolution of polar meteorology in both hemispheres, beginning with measure- ments made during early expeditions and concluding with the recent decades in which polar meteorology has been central to global challenges such as the ozone hole, weather prediction, and climate change. Whereas the 1800s and early 1900s provided data from expeditions and only a few subarctic stations, the past 100 years have seen great advances in the observational network and corresponding understanding of the meteorology of the polar regions. For example, a persistent view in the early twentieth century was of an Arctic Ocean dominated by a permanent high pressure cell, a glacial anticyclone. With increased observations, by the 1950s it became apparent that, while anticyclones are a common feature of the Arctic circulation, cyclones are frequent and may be found anywhere in the Arctic. Technology has benefited polar meteorology through advances in in- strumentation, especially autonomously operated instruments. Moreover, satellite remote sensing and com- puter models revolutionized polar meteorology.
    [Show full text]
  • For Other Uses, See Ship (Disambiguation). in Modern Parlance A
    Ship From Wikipedia, the free encyclopedia (Redirected from Ships) For other uses, see Ship (disambiguation). Italian full-rigged ship Amerigo Vespucci in New York Harbor, 1976 In modern parlance a ship has been any large buoyant watercraft. Ships are generally distinguished from boats based on size, shape andcargo or passenger capacity. Ships are used on lakes, seas, and rivers for a variety of activities, such as the transport of people or goods,fishing, entertainment, public safety, and warfare. Historically, a "ship" was a sailing vessel with at least three square-rigged masts and a full bowsprit. Ships and boats have developed alongside humanity. In armed conflict and in daily life they have become an integral part of modern commercial and military systems. Fishing boats are used by millions of fishermen throughout the world. Military forces operate vessels for combat and to transport and support forces ashore. Commercial vessels, nearly 35,000 in number, carried 7.4 billion tons of cargo in 2007.[1] As of 2011, there are about 104,304 ships with IMO numbers in the world.[2] Ships were always a key in history's great explorations and scientific and technological development. Navigators such as Zheng He spread such inventions as the compass and gunpowder. Ships have been used for such purposes as colonization and the slave trade, and have served scientific, cultural, and humanitarian needs. After the 16th century, new crops that had come from and to the Americas via the European seafarers significantly contributed to the world's population growth.[3] Maritime transport has shaped the world's economy into today's energy-intensive pattern.
    [Show full text]
  • Guide to the Science of Climate Change in the 21St Century
    January 11, 2021 Guide to the Science of Climate Change st in the 21 Century Chapter 14 Modern Instrumental Period David H. Manz PhD., P. Eng., AOE, FCAE 2020 Eco-print, “Monet’s Garden #2”, Nora Manz 2020 Table of Contents Chapter 14 Modern Instrumental Period 14.1 Introduction 14.2 Instrumental temperature record 14.3 Modern instrumentation 14.4 Satellites 14.4 Information support List of Figures Figure 14.1 Global average temperature change – 1850 to present. Figure 14.2 Global Observing System – WMO https://public.wmo.int/en/programmes/global- observing-system Figure 14.3 Modern surface weather station, U.S. Climate Reference Network Station, Ithaca, New York. Figure 14.4 Weather ship MS Polarfront at sea – decommissioned in 2009. Note that weatherships are no longer used. Figure 14.5 Weather buoy operated by the NOAA National Buoy Center. Figure 14.6 Weather Station – remote land based. Figure 14.7 Antarctic automatic weather station – part of the automatic weather stations project AWS in Antarctica. Figure 14.8 Commercial automatic weather observation station AWOS. Figure 14.9 Remote manned weather stations. Figure 14.10 Weather balloons with radiosonde. Figure 14.11 NASA Earth science spacecraft and instruments in orbit. Figure 14.12 GOES-8, a United States weather satellite of the meteorological-satellite service. https://en.wikipedia.org/wiki/Weather_satellite 2 December 12, 2020 – Fi�h Anniversary of the Paris Agreement Guide to the Science of Climate Change Figure 14.13 Global precipitation measurement from NASA GES DISC satellite https://www.nasa.gov/mission_pages/GPM/overview/index.html Figure 14.14 Infrared Sounder on NASA’s Aqua Satellite.
    [Show full text]