GPS and Leap Seconds Time to Change?

Total Page:16

File Type:pdf, Size:1020Kb

GPS and Leap Seconds Time to Change? INNOVATION GPS and Leap Seconds Time to Change? Dennis D. McCarthy, U.S. Naval Observatory William J. Klepczynski, Innovative Solutions International Since ancient times, we have used the Just as leap years keep our calendar approxi- seconds. While resetting the GLONASS Earth’s rotation to regulate our daily mately synchronized with the Earth’s orbit clocks, the system is unavailable for naviga- activities. By noticing the approximate about the Sun, leap seconds keep precise tion service because the clocks are not syn- position of the sun in the sky, we knew clocks in synchronization with the rotating chronized. If worldwide reliance on satellite how much time was left for the day’s Earth, the traditional “clock” that humans navigation for air transportation increases in hunting or farming, or when we should have used to determine time. Coordinated the future, depending on a system that may stop work to eat or pray. First Universal Time (UTC), created by adjusting not be operational during some critical areas sundials, water clocks, and then International Atomic Time (TAI) by the of flight could be a difficulty. Recognizing mechanical clocks were invented to tell appropriate number of leap seconds, is the this problem, GLONASS developers plan to time more precisely by essentially uniform time scale that is the basis of most significantly reduce the outage time with the interpolating from noon to noon. civil timekeeping in the world. The concept next generation of satellites. As mechanical clocks became of a leap second was introduced to ensure Navigation is not the only service affected increasingly accurate, we discovered that UTC would not differ by more than 0.9 by leap seconds. Spread-spectrum systems that the Earth does not rotate “like second from UT1, the time determined by the also rely on time synchronization for effec- clockwork,” but actually has a slightly rotation of the Earth — a choice made pri- tive communications. When sychronization nonconstant rotation rate. In addition marily to meet the requirements for celestial is lost, so too is coherent communication. to periodic and irregular variations navigation. Thus, while a leap second is being intro- caused by atmospheric winds and the To determine longitude and latitude using duced, and until sychronization is estab- interaction between the Earth’s core a sextant and observations of stars, one needs lished, communications can be disrupted and the mantle, the tidal interaction to know UT1 at the instant of the observa- between some systems. of the Earth and the Moon causes a tions. An error of one second in time could In view of these emerging problems, user secular slowing down of the Earth’s translate into an error of about 500 meters in dissatisfaction with leap seconds is beginning rotation. So rather than use the position. Celestial navigation was one of the to surface, and concern is growing that users variable time scale based on the major navigation techniques used throughout will construct time scales independent of Earth’s rotation, we now use time the world in 1972, when the first leap second UTC that they perceive are more suited to scales based on extraordinarily was introduced. With the recent proliferation their individual requirements. This would precise atomic time, the basis for all of satellite navigation, however, it is appro- lead to an increased number of nonstandard the world’s civil time systems — priate to reconsider this historical position, as time scales. Coordinated Universal Time (UTC). the leap second may in fact be detrimental to Although we have accurate estimates of However, because of the desire some systems, possibly creating life-threat- the deceleration of the Earth’s rotation, sig- to keep UTC more or less in ening situations. nificant variations prevent the prediction of synchronization with the Earth’s Modern commercial transportation sys- leap seconds beyond a few months in rotation as an aid in determining tems now almost entirely depend on satellite advance. This inability to predict leap sec- navigation fixes using astronomical navigation systems. In the future, commer- onds, coupled with the growing urgency for a observations, leap seconds are added cial aviation is expected to rely on various uniform time scale without discontinuities, to UTC — currently about every 18 augmentation systems to improve satellite makes it appropriate to re-examine the leap months. navigation accuracy, reliability, integrity, second’s role. Later in this article, we will In contrast, the time scale used to and availability beyond current capabil- outline several possible scenarios for dealing regulate the Global Positioning System ities. The introduction of a leap second with leap seconds in the future, but first, let’s — GPS Time — is a “pure” atomic does not affect GPS operations because its review how the present system came to be. time scale without leap seconds. In time system is GPS Time, which is not this month’s column, Drs. Dennis adjusted to account for leap seconds. But A BRIEF HISTORY McCarthy and William Klepczynski GPS does provide UTC by transmitting the Historically, humans used astronomical phe- suggest that the practice of adding leap necessary data in its navigation message, nomena to keep time. The passage of the Sun seconds to UTC be done away with or permitting a receiver to compute UTC from across a north–south (meridian) line deter- at least modified, as more and more GPS Time. mined noon. Until 1960, the average solar navigators adopt Global Navigation By contrast, GLONASS uses UTC as its day was used as the basis for timekeeping, Satellite Systems as their primary time reference (actually UTC ` 3 hours with the second defined as 1/86,400 of the means of positioning. which is Moscow Time), and so its satellite mean solar day. Under this system, the length clocks must be reset to account for any leap of the second depended on the Earth’s rate of 50 GPS WORLD November 1999 www.gpsworld.com INNOVATION rotation, because its rotation causes the Sun to appear to move across the sky. 80 During the mid-1930s, astronomers con- cluded the Earth did not rotate uniformly, basing their findings on measurements of the 60 most precise clocks then available. We now know that a variety of physical phenomena affect the Earth’s rotational speed. This 40 caused the second to be redefined in 1960 in terms of the Earth’s orbital motion around 20 the Sun. The new second was called the “Ephemeris” second and the time scale 0 derived from this definition was called (seconds) T Ephemeris Time (ET). D The name called attention to the fact that -20 the definition depended on the position and motion (ephemeris) of the Sun (or Moon) used in the astronomical determination of -40 time. It was originally thought that the new definition would provide a more uniform -60 measure of the second’s length. ET is very 1600 1700 1800 1900 2000 difficult to measure and observe, however, Year requiring a series of accurate astronomical observations stretching over years. In 1967, the second was again redefined, Figure 1. Observations and quadratic fit of the difference between a uniform time this time in terms of the resonance frequency scale and one based on the Earth’s rotation of the cesium atom, which had already been calibrated with respect to ET. By the early we would have to add some time to the face can vary either way. So far, all leap seconds 1960s, cesium frequency standards became of our atomic clock, which is exactly what have been positive. known as reliable, uniform, and accurate we do when we add a leap second to our Astronomical observations show a near- clocks. Defining the second this way pro- clocks. We are bringing the faces of our lab- constant deceleration of the Earth’s rotation vided a uniform standard that easily could be oratory clocks back into agreement with rate caused by the braking action of the tides. measured in a laboratory with greater preci- the time kept by the rotating Earth, so that This deceleration explains why the length of sion and accuracy than any astronomical sunrise will occur at the “correct” time from the astronomical day is approximately two phenomena. year to year. milliseconds longer today than at the begin- Increasing Accuracy. Subsequently, ET was The Move to Cesium. With the introduction of ning of the twentieth century. With the differ- superseded by a set of dynamical time scales the cesium atom–based definition of the sec- ence between UTC and UT1 growing at the defined to meet special relativistic require- ond, it was known that there would be a time rate of two milliseconds per day, or 0.7 sec- ments. At the level of accuracy with which varying discrepancy between a clock running ond per year, currently about one leap second ET could be determined (approximately at a uniform rate and a theoretical one using a per year must be inserted in UTC. 0.001 second), these new time scales are second defined solely by the Earth’s rotation The astronomical observations provide a equivalent to ET and include Terrestrial rate. Beginning in 1961, the Bureau Interna- clear estimate of the magnitude of the decel- Dynamical Time (TDT), Barycentric tional de l’Heure (the forerunner of the Inter- eration of the Earth’s rotation rate. Figure 1 Dynamical Time (TDB), Terrestrial Time national Earth Rotation Service) accounted combines data from as far back as the 1600s (TT), Geocentric Coordinate Time (TCG), for these observed variations by making with data recently acquired using modern and Barycentric Coordinate Time (TCB). small adjustments, on the order of a few mil- space geodetic techniques to show the The advantage of these scales over ET is the liseconds, to our civil time clocks and by difference between astronomical time and incorporation of relativistic effects and a making occasional small adjustments to the uniform time, along with a parabola fit to the defined relationship to atomic time.
Recommended publications
  • Ast 443 / Phy 517
    AST 443 / PHY 517 Astronomical Observing Techniques Prof. F.M. Walter I. The Basics The 3 basic measurements: • WHERE something is • WHEN something happened • HOW BRIGHT something is Since this is science, let’s be quantitative! Where • Positions: – 2-dimensional projections on celestial sphere (q,f) • q,f are angular measures: radians, or degrees, minutes, arcsec – 3-dimensional position in space (x,y,z) or (q, f, r). • (x,y,z) are linear positions within a right-handed rectilinear coordinate system. • R is a distance (spherical coordinates) • Galactic positions are sometimes presented in cylindrical coordinates, of galactocentric radius, height above the galactic plane, and azimuth. Angles There are • 360 degrees (o) in a circle • 60 minutes of arc (‘) in a degree (arcmin) • 60 seconds of arc (“) in an arcmin There are • 24 hours (h) along the equator • 60 minutes of time (m) per hour • 60 seconds of time (s) per minute • 1 second of time = 15”/cos(latitude) Coordinate Systems "What good are Mercator's North Poles and Equators Tropics, Zones, and Meridian Lines?" So the Bellman would cry, and the crew would reply "They are merely conventional signs" L. Carroll -- The Hunting of the Snark • Equatorial (celestial): based on terrestrial longitude & latitude • Ecliptic: based on the Earth’s orbit • Altitude-Azimuth (alt-az): local • Galactic: based on MilKy Way • Supergalactic: based on supergalactic plane Reference points Celestial coordinates (Right Ascension α, Declination δ) • δ = 0: projection oF terrestrial equator • (α, δ) = (0,0):
    [Show full text]
  • WWVB: a Half Century of Delivering Accurate Frequency and Time by Radio
    Volume 119 (2014) http://dx.doi.org/10.6028/jres.119.004 Journal of Research of the National Institute of Standards and Technology WWVB: A Half Century of Delivering Accurate Frequency and Time by Radio Michael A. Lombardi and Glenn K. Nelson National Institute of Standards and Technology, Boulder, CO 80305 [email protected] [email protected] In commemoration of its 50th anniversary of broadcasting from Fort Collins, Colorado, this paper provides a history of the National Institute of Standards and Technology (NIST) radio station WWVB. The narrative describes the evolution of the station, from its origins as a source of standard frequency, to its current role as the source of time-of-day synchronization for many millions of radio controlled clocks. Key words: broadcasting; frequency; radio; standards; time. Accepted: February 26, 2014 Published: March 12, 2014 http://dx.doi.org/10.6028/jres.119.004 1. Introduction NIST radio station WWVB, which today serves as the synchronization source for tens of millions of radio controlled clocks, began operation from its present location near Fort Collins, Colorado at 0 hours, 0 minutes Universal Time on July 5, 1963. Thus, the year 2013 marked the station’s 50th anniversary, a half century of delivering frequency and time signals referenced to the national standard to the United States public. One of the best known and most widely used measurement services provided by the U. S. government, WWVB has spanned and survived numerous technological eras. Based on technology that was already mature and well established when the station began broadcasting in 1963, WWVB later benefitted from the miniaturization of electronics and the advent of the microprocessor, which made low cost radio controlled clocks possible that would work indoors.
    [Show full text]
  • A Study of Ancient Khmer Ephemerides
    A study of ancient Khmer ephemerides François Vernotte∗ and Satyanad Kichenassamy** November 5, 2018 Abstract – We study ancient Khmer ephemerides described in 1910 by the French engineer Faraut, in order to determine whether they rely on observations carried out in Cambodia. These ephemerides were found to be of Indian origin and have been adapted for another longitude, most likely in Burma. A method for estimating the date and place where the ephemerides were developed or adapted is described and applied. 1 Introduction Our colleague Prof. Olivier de Bernon, from the École Française d’Extrême Orient in Paris, pointed out to us the need to understand astronomical systems in Cambo- dia, as he surmised that astronomical and mathematical ideas from India may have developed there in unexpected ways.1 A proper discussion of this problem requires an interdisciplinary approach where history, philology and archeology must be sup- plemented, as we shall see, by an understanding of the evolution of Astronomy and Mathematics up to modern times. This line of thought meets other recent lines of research, on the conceptual evolution of Mathematics, and on the definition and measurement of time, the latter being the main motivation of Indian Astronomy. In 1910 [1], the French engineer Félix Gaspard Faraut (1846–1911) described with great care the method of computing ephemerides in Cambodia used by the horas, i.e., the Khmer astronomers/astrologers.2 The names for the astronomical luminaries as well as the astronomical quantities [1] clearly show the Indian origin ∗F. Vernotte is with UTINAM, Observatory THETA of Franche Comté-Bourgogne, University of Franche Comté/UBFC/CNRS, 41 bis avenue de l’observatoire - B.P.
    [Show full text]
  • Ephemeris Time, D. H. Sadler, Occasional
    EPHEMERIS TIME D. H. Sadler 1. Introduction. – At the eighth General Assembly of the International Astronomical Union, held in Rome in 1952 September, the following resolution was adopted: “It is recommended that, in all cases where the mean solar second is unsatisfactory as a unit of time by reason of its variability, the unit adopted should be the sidereal year at 1900.0; that the time reckoned in these units be designated “Ephemeris Time”; that the change of mean solar time to ephemeris time be accomplished by the following correction: ΔT = +24°.349 + 72s.318T + 29s.950T2 +1.82144 · B where T is reckoned in Julian centuries from 1900 January 0 Greenwich Mean Noon and B has the meaning given by Spencer Jones in Monthly Notices R.A.S., Vol. 99, 541, 1939; and that the above formula define also the second. No change is contemplated or recommended in the measure of Universal Time, nor in its definition.” The ultimate purpose of this article is to explain, in simple terms, the effect that the adoption of this resolution will have on spherical and dynamical astronomy and, in particular, on the ephemerides in the Nautical Almanac. It should be noted that, in accordance with another I.A.U. resolution, Ephemeris Time (E.T.) will not be introduced into the national ephemerides until 1960. Universal Time (U.T.), previously termed Greenwich Mean Time (G.M.T.), depends both on the rotation of the Earth on its axis and on the revolution of the Earth in its orbit round the Sun. There is now no doubt as to the variability, both short-term and long-term, of the rate of rotation of the Earth; U.T.
    [Show full text]
  • An Introduction to Orbit Dynamics and Its Application to Satellite-Based Earth Monitoring Systems
    19780004170 NASA-RP- 1009 78N12113 An introduction to orbit dynamics and its application to satellite-based earth monitoring systems NASA Reference Publication 1009 An Introduction to Orbit Dynamics and Its Application to Satellite-Based Earth Monitoring Missions David R. Brooks Langley Research Center Hampton, Virginia National Aeronautics and Space Administration Scientific and Technical Informalion Office 1977 PREFACE This report provides, by analysis and example, an appreciation of the long- term behavior of orbiting satellites at a level of complexity suitable for the initial phases of planning Earth monitoring missions. The basic orbit dynamics of satellite motion are covered in detail. Of particular interest are orbit plane precession, Sun-synchronous orbits, and establishment of conditions for repetitive surface coverage. Orbit plane precession relative to the Sun is shown to be the driving factor in observed patterns of surface illumination, on which are superimposed effects of the seasonal motion of the Sun relative to the equator. Considerable attention is given to the special geometry of Sun- synchronous orbits, orbits whose precession rate matches the average apparent precession rate of the Sun. The solar and orbital plane motions take place within an inertial framework, and these motions are related to the longitude- latitude coordinates of the satellite ground track through appropriate spatial and temporal coordinate systems. It is shown how orbit parameters can be chosen to give repetitive coverage of the same set of longitude-latitude values on a daily or longer basis. Several potential Earth monitoring missions which illus- trate representative applications of the orbit dynamics are described. The interactions between orbital properties and the resulting coverage and illumina- tion patterns over specific sites on the Earth's surface are shown to be at the heart of satellite mission planning.
    [Show full text]
  • QUICK REFERENCE GUIDE Latitude, Longitude and Associated Metadata
    QUICK REFERENCE GUIDE Latitude, Longitude and Associated Metadata The Property Profile Form (PPF) requests the property name, address, city, state and zip. From these address fields, ACRES interfaces with Google Maps and extracts the latitude and longitude (lat/long) for the property location. ACRES sets the remaining property geographic information to default values. The data (known collectively as “metadata”) are required by EPA Data Standards. Should an ACRES user need to be update the metadata, the Edit Fields link on the PPF provides the ability to change the information. Before the metadata were populated by ACRES, the data were entered manually. There may still be the need to do so, for example some properties do not have a specific street address (e.g. a rural property located on a state highway) or an ACRES user may have an exact lat/long that is to be used. This Quick Reference Guide covers how to find latitude and longitude, define the metadata, fill out the associated fields in a Property Work Package, and convert latitude and longitude to decimal degree format. This explains how the metadata were determined prior to September 2011 (when the Google Maps interface was added to ACRES). Definitions Below are definitions of the six data elements for latitude and longitude data that are collected in a Property Work Package. The definitions below are based on text from the EPA Data Standard. Latitude: Is the measure of the angular distance on a meridian north or south of the equator. Latitudinal lines run horizontal around the earth in parallel concentric lines from the equator to each of the poles.
    [Show full text]
  • What Time Is It?
    The Astronomical League A Federation of Astronomical Societies Astro Note E3 – What Time Is It? Introduction – There are many methods used to keep time, each having its own special use and advantage. Until recently, when atomic clocks became available, time was reckoned by the Earth's motions: one rotation on its axis was a "day" and one revolution about the Sun was a "year." An hour was one twenty-fourth of a day, and so on. It was convenient to use the position of the Sun in the sky to measure the various intervals. Apparent Time This is the time kept by a sundial. It is a direct measure of the Sun's position in the sky relative to the position of the observer. Since it is dependent on the observer's location, it is also a local time. Being measured according to the true solar position, it is subject to all the irregularities of the Earth's motion. The reference time is 12:00 noon when the true Sun is on the observer's meridian. Mean Time Many of the irregularities in the Earth's motion are due to its elliptical orbit. In order to add some consistency to the measure of time, we use the concept of mean time. Mean time uses the position of a fictitious "mean Sun" which moves smoothly and uniformly across the sky and is insensitive to the irregularities of the Earth’s motion. A mean solar day is 24 hours long. The "Equation of Time," tabulated in almanacs and represented on maps by the analemma, provides the correction between mean and apparent time to allow for the eccentricity of the Earth's orbit.
    [Show full text]
  • An Atomic Physics Perspective on the New Kilogram Defined by Planck's Constant
    An atomic physics perspective on the new kilogram defined by Planck’s constant (Wolfgang Ketterle and Alan O. Jamison, MIT) (Manuscript submitted to Physics Today) On May 20, the kilogram will no longer be defined by the artefact in Paris, but through the definition1 of Planck’s constant h=6.626 070 15*10-34 kg m2/s. This is the result of advances in metrology: The best two measurements of h, the Watt balance and the silicon spheres, have now reached an accuracy similar to the mass drift of the ur-kilogram in Paris over 130 years. At this point, the General Conference on Weights and Measures decided to use the precisely measured numerical value of h as the definition of h, which then defines the unit of the kilogram. But how can we now explain in simple terms what exactly one kilogram is? How do fixed numerical values of h, the speed of light c and the Cs hyperfine frequency νCs define the kilogram? In this article we give a simple conceptual picture of the new kilogram and relate it to the practical realizations of the kilogram. A similar change occurred in 1983 for the definition of the meter when the speed of light was defined to be 299 792 458 m/s. Since the second was the time required for 9 192 631 770 oscillations of hyperfine radiation from a cesium atom, defining the speed of light defined the meter as the distance travelled by light in 1/9192631770 of a second, or equivalently, as 9192631770/299792458 times the wavelength of the cesium hyperfine radiation.
    [Show full text]
  • Day-Ahead Market Enhancements Phase 1: 15-Minute Scheduling
    Day-Ahead Market Enhancements Phase 1: 15-minute scheduling Phase 2: flexible ramping product Stakeholder Meeting March 7, 2019 Agenda Time Topic Presenter 10:00 – 10:10 Welcome and Introductions Kristina Osborne 10:10 – 12:00 Phase 1: 15-Minute Granularity Megan Poage 12:00 – 1:00 Lunch 1:00 – 3:20 Phase 2: Flexible Ramping Product Elliott Nethercutt & and Market Formulation George Angelidis 3:20 – 3:30 Next Steps Kristina Osborne Page 2 DAME initiative has been split into in two phases for policy development and implementation • Phase 1: 15-Minute Granularity – 15-minute scheduling – 15-minute bidding • Phase 2: Day-Ahead Flexible Ramping Product (FRP) – Day-ahead market formulation – Introduction of day-ahead flexible ramping product – Improve deliverability of FRP and ancillary services (AS) – Re-optimization of AS in real-time 15-minute market Page 3 ISO Policy Initiative Stakeholder Process for DAME Phase 1 POLICY AND PLAN DEVELOPMENT Issue Straw Draft Final June 2018 July 2018 Paper Proposal Proposal EIM GB ISO Board Implementation Fall 2020 Stakeholder Input We are here Page 4 DAME Phase 1 schedule • Third Revised Straw Proposal – March 2019 • Draft Final Proposal – April 2019 • EIM Governing Body – June 2019 • ISO Board of Governors – July 2019 • Implementation – Fall 2020 Page 5 ISO Policy Initiative Stakeholder Process for DAME Phase 2 POLICY AND PLAN DEVELOPMENT Issue Straw Draft Final Q4 2019 Q4 2019 Paper Proposal Proposal EIM GB ISO Board Implementation Fall 2021 Stakeholder Input We are here Page 6 DAME Phase 2 schedule • Issue Paper/Straw Proposal – March 2019 • Revised Straw Proposal – Summer 2019 • Draft Final Proposal – Fall 2019 • EIM GB and BOG decision – Q4 2019 • Implementation – Fall 2021 Page 7 Day-Ahead Market Enhancements Third Revised Straw Proposal 15-MINUTE GRANULARITY Megan Poage Sr.
    [Show full text]
  • Building the Bridge Between the First and Second Year Experience: a Collaborative Approach to Student Learning and Development STEP
    Building the bridge between the first and second year experience: A collaborative approach to student learning and development STEP Introductions STEP Agenda for Today • Share research and theory that shapes first and second year programs • Differentiate programs, interventions, and support that should be targeted at first year students, second year students, or both • Think about your own department and how to work differently with first and second-year students • Review structure of FYE and STEP at Ohio State and where your office can support existing efforts STEP Learning Outcomes • Participants will reflect on and articulate what services, resources, and programming currently exist in their department for first and/or second year students. • Participants will articulate the key salient needs and developmental milestones that often distinguish the second year experience from the first. • Participants will be able to utilize at least one strategy for curriculum differentiation that will contribute to a more seamless experiences for students between their first and second year. Foundational Research that Informs FYE and STEP STEP Developmental Readiness and Sequencing • Developmental Readiness: “The ability and motivation to attend to, make meaning of, and appropriate new knowledge into one’s long term memory structures” (Hannah & Lester, 2009). • Sequencing: The order and structure in which people learn new skill sets (Hannah & Avolio, 2010). • Scaffolding: Support given during the learning process which is tailored to the needs of an
    [Show full text]
  • International Earth Rotation and Reference Systems Service (IERS) Provides the International Community With
    The Role of the IERS in the Leap Second Brian Luzum Chair, IERS Directing Board Background The International Earth Rotation and Reference Systems Service (IERS) provides the international community with: • the International Celestial Reference System and its realization, the International Celestial Reference Frame (ICRF); • the International Terrestrial Reference System and its realization, the International Terrestrial Reference Frame (ITRF); • Earth orientation parameters (EOPs) that are used to transform between the ICRF and the ITRF; • Conventions (i.e., standards, models, and constants) used in generating and using reference frames and EOPs; • Geophysical data to study and understand variations in the reference frames and the Earth’s orientation. The IERS was created in 1987 and began operations on 1 January 1988. It continued much of the tasking of the Bureau International de l’Heure (BIH), which had been created early in the 20th century. It is responsible to the International Astronomical Union (IAU) and the International Union of Geodesy and Geophysics (IUGG). For more than twenty-five years, the IERS has been providing for the reference frame and EOP needs of a variety of users. Time The IERS has an important role in determining when the leap seconds are to be inserted and the dissemination of information regarding leap seconds. In order to understand this role, it is important to realize some things regarding time. For instance, there are two different kinds of “time” being related: (1) a uniform time, now based on atomic clocks and (2) “time” based on the variable rotation of the Earth. The differences between uniform time and Earth rotation “time” only became apparent in the 1930s with the improvements in clock technology.
    [Show full text]
  • September 2019
    JUDICIAL COUNCIL OF CALIFORNIA 455 Golden Gate Avenue . San Francisco, California 94102-3688 www.courts.ca.gov REPORT TO THE JUDICI AL COUNCIL For business meeting on: September 23–24, 2019 Title Agenda Item Type Judicial Workload Assessment: 2018 Judicial Action Required Workload Study Updated Caseweights Effective Date Rules, Forms, Standards, or Statutes Affected September 24, 2019 None Date of Report Recommended by September 10, 2019 Workload Assessment Advisory Committee Hon. Lorna A. Alksne, Chair Contact Judicial Council staff Kristin Greenaway, 415-865-7832 Kristin Greenaway, Supervising Research [email protected] Analyst Office of Court Research Executive Summary The Workload Assessment Advisory Committee (WAAC) recommends that the Judicial Council adopt the proposed Judicial Workload Study updated model parameters that are used as part of the formula for assessing judicial need in the trial courts. The council previously approved the Judicial Workload Study in 2001 and 2011; the current update accounts for changes in the law and practice that have affected judicial workload since the last study update in 2011. The recommendation also reflects direction from the Judicial Council, at its July 18, 2019 meeting, to perform additional analysis to ensure the model best represents courts of all sizes. Further, WAAC recommends that the council approve an updated Judicial Needs Assessment per Government Code section 69614(c)(1) based on the new judicial workload measures and the established methodology for prioritization of judgeships. The updated needs assessment would replace a preliminary version that was completed in 2018 using workload measures developed in 2011. Recommendation The Workload Assessment Advisory Committee recommends that the Judicial Council: 1.
    [Show full text]