Mexico United States

Total Page:16

File Type:pdf, Size:1020Kb

Mexico United States 1 1 United States Mexico 2 3 4 Figure 1. Geographical area of northwestern Mexico with topographic contours (shaded, m) given in the 5 vertical bar. Specific locations mentioned throughout the text are the states of Nayarit (NAY), Sinaloa 6 (SIN), Sonora (SON), Baja California (BC), and Baja California Sur (BCS). Circled letters are the five 7 largest communities in BCS and SIN, shown in Table 1. Dots represent landfall positions from tropical 8 cyclones during the period 1969–2006. The dashed box outlines the area shown in Figs. 12 and 15. 9 1 2 11 Figure 2. Tracks of tropical cyclones that, during the seasons 1969–2006, made first landfall over the (a) Baja California Peninsula and (b) Mainland Mexico. Thick lines are tropical cyclones from 2006. Temporal frequency (percentage) of landfall strikes is shown in upper-right inserts. The lower-left lists provide the five strongest hurricanes at landfall: name, year, and maximum winds in m s-1 (Saffir-Simpson scale category). Small dots are initial locations with corresponding labels (first letter name and two-digit 2 year). The large dot represents Isla Socorro. 3 13 15 Figure 3. Mean streamlines at the 500-hPa level from the NCEP-NCAR reanalysis for selected cases from Fig. 2. Tropical cyclones at time of landfall over the (a) Baja California peninsula and (b) the mainland are considered. Dashed line is the 10 m s-1 wind speed contour at 500-hPa. The black dots indicate corresponding mean position of TCs from the best track, plus signs are 12 and 24 hours before and after lnadfall. Shading represents the 850-200 hPa wind shear with light, intermediate and dark tones indicating -1 values above 10, 20 and 30 m s respectively. 3 4 16 Figure 4. Tracks of tropical cyclones John (28 August– 4 September), Lane (13-17 September), and Paul (21-26 October) in 2006. Positions are marked every 6 hours, numbers are dates of fixes at 00:00 UTC with final positions given by lower-case initials. Location of maximum intensity (MAX) and recurvature initiation (REC) are indicated. Inserts show sustained wind speed (m s-1), maximum intensity, and time of landfall (vertical line). Dashed lines are the tropical storm (17 m s-1) and hurricane (33 m s-1) intensity thresholds. 4 5 18 20 Figure 5. Rainfall accumulations from TRMM during selected periods and during the development of tropical cyclones in 2006. The vertical bar indicates the amount of accumulations (mm). Best-track positions are indicated by circles (John), plus signs (Lane), and crosses (Paul) at 6-hour intervals. 5 6 22 24 Figure 6. GOES-11 infrared and water vapor imagery at landfall. Infrared images are from (a) Hurricane John, (b) Hurricane Lane, and (c) Tropical Depression Paul in 2006. Landfall positions are symbols as in Fig. 4 and the vertical bar indicates a calibrated scale of cloud top temperature (°C). Simultaneous water vapor imagery is at the right column with precipitable water (mm) from upper-air soundings. Crosses represent missing soundings. 6 7 25 Figure 7. North American Regional Reanalysis fields at 00:00 UTC from (a-c) 31 August–2 September, (d-f) 15–18 September, and (g-i) 24–26 October 2006. Streamlines are at the 500-hPa level. Shading represents the 850–200 hPa horizontal wind shear with light, intermediate and dark tones representing values above 10, 20, and 30 m s-1, respectively. Dashed lines are wind speeds at 20 and 30 m s-1. Thick lines are the locations of the vertical cross sections shown in Fig. 11. Black dots are the corresponding tropical cyclone positions at 00:00 UTC as well as 12 hours before and after. Colored dots are corresponding positions from tropical cyclones Kristy (blue) and Miriam (red). 7 8 26 Figure. 8. Reflectivity (dBZ) from the Cabo San Lucas, Baja California Sur, radar at (a) 05:53 UTC 1, September, (b) 18:42 UTC, 1 September, and (c) 02:03 UTC 2 September. Rain rate (mm h-1) image from the Guasave, Sinaloa, radar at (d) 12:15 UTC 2 September. Radar stations are located at the white dots. 8 9 1 Figure 9. Total rainfall (mm) in Baja California Sur from the period 31 August–4 September 2006. 27 Top ten reports are circled and shown in Table 2. Best-track positions (large dots) and intensities (Hurricane=HR, Tropical Storm=TS, and Tropical Depression=TD) are indicated. Terrain elevations (shaded) are at 300-m intervals. Asterisk is the landfall site for John and triangles are the four strongest hurricanes (name initial and year) from Fig. 2a. 9 10 37 Figure 10. Radar images of (a) reflectivity (dBZ) from Cabo San Lucas, Baja California Sur, at 12:03UTC 16 September and (b) rain rate (mm h-1) from Guasave, Sinaloa, at 19:17 UTC 16 September 2006. The radars are located at the white dots. (c) GOES-11 visible image at 19:15 UTC 16 Sep. 10 a 11 b c 38 Figure 11. Cross section from the NARR at (a) 00:00 UTC 15 September, (b) 00:00 UTC 16 September and (c) 00:00 UTC 18 September 2006. Vertical axis is pressure from 100-1000 hPa. Shading is mixing ratio (g kg-1) with contour interval given in the bar. Isotachs (contour interval 5 m s-1) of zonal wind component given by the thick (positive) and dashed (negative) lines. Geographical location of cross sections is indicated in Figs. 7d-f. 11 12 45 47 Figure 12. Total rainfall (mm) in Sinaloa from the period 14–16 September 2006. Top -ten reports are circled and shown in Table 3. Best-track positions (large dots) and intensities (Hurricane=HR, Tropical Storm=TS, and Tropical Depression=TD) are indicated. Terrain elevations (shaded) are at 600-m intervals. Asterisk is the landfall site for Lane and triangles (name initial and year) are three strongest hurricanes from Fig. 2b. 12 a 13 49 51 b Figure 13. GOES-11 visible imagery at (a) 20:45 UTC 24 October and (b) 14:45 UTC 25 October 2006. The circles represent the low-level circulation associated with Tropical Storm Paul. 13 14 53 Figure 14. Time series of winds and mixing ratio from upper-air soundings for the period 00:0055 UTC 22 October through 00:00 UTC 29 October 2006. Full wind barbs indicate 5.0 m s-1 and half barbs 2.5 m s-1. Mixing ratio (g kg-1) is shaded and contour intervals are given in the bar. Vertical axis represents pressure levels from 1000 to 100 hPa. 14 15 57 59 Figure 15. Total rainfall (mm) in Sinaloa from the period 24–26 October 2006. Top -ten reports are circled and shown in Table 4. Best-track positions (large dots) and intensities (Tropical Storm=TS, and Tropical Depression=TD) are indicated. Terrain elevations (shaded) are at 600-m intervals. Asterisk is the landfall site for Paul. 15 16 61 63 Figure 16. Best-track and official forecast positions for John, Lane, and Paul. Initial dates of forecasts are given in the lower-left inserts (symbol, day, and month). Forecasts are valid at 12, 24, 36, 48, 72, 96, and 120 hours. Thick and thin (with dots) lines represents best tracks. Black dots are locations of upper- air stations in Mexico. Numbers indicate released soundings at 00:00 UTC (left from slash) and 12:00 UTC (right from slash) during the three days covered by each case. Insert table indicates track errors (km) at valid times the bold number representing maximum error per time. 16 17 64 -1 65 Figure 17. Mean track (aa, km) and intensity (bb, m sP )P errors from official forecasts for tropical 66 cyclones John, Lane, and Paul. Mean errors from all tropical cyclones from the eastern North 67 Pacific basin, during the season of 2006, are indicated (thick line). Data sources is the are forecast 68 verification reportstatistics byfrom Franklin (2007, Table 13). 17 18 69 Figure 18. Global Forecast System forecast (FCST) and analysis (ANL) fields at 00:00 UTC (a, d) 2 September, (b-e) 18:00 UTC 16 September, and (c-f) 00:00 UTC 26 October, 2006. Streamlines are at the 500- hPa level. Shading represents 850–200 hPa wind shear with light, intermediate, and dark tones representing values above 10, 20, and 30 m s-1, respectively. Thick arrows are an estimate of the steering flow. Black dots are tropical cyclone positions from the best track. Circles and dots are positions from Kristy (blue) and Miriam (red). 18 19 Figure 19. Best-track and official forecast positions from tropical cyclones making landfall in Baja California (top panels) and mainland Mexico (bottom panels) during the period 1998-2005. Forecasts are valid at 12, 24, 36, 48, 72, 96, and 120 hours. Forecasts were issued, approximately, 72- (plus signs), 48- (circles), and 24- (crosses) hours prior to landfall. Thick line represents the best track and black dots are locations of available upper-air observations. 19 20 70 71 Table 1. Population (inhabitants) from the five largest cities in the states of Baja California Sur and 72 Sinaloa, Mexico. Source of data INEGI (2005). The city identification (CI) is used to show the 73 corresponding geographical location in Fig. 1. 74 ____________________________________________________________ 75 CI Baja California Sur CI Sinaloa. 76 ____________________________________________________________ 77 Baja California Sur (512,170) Sinaloa (2,608,442) 78 79 A La Paz (189,176) A Culiacán (605,304) 80 B Cabo San Lucas (56,811) B Mazatlán (352,471) 81 C San José del Cabo (48,518) C Los Mochis (231,977) 82 D Ciudad Constitución (37,221) D Guasave (66,793) 83 E Loreto (10,283) E Guamúchil (61,862) 84 ____________________________________________________________ 85 86 Number of inhabitants is indicated in parenthesis.
Recommended publications
  • P2h.8 Landfalling Tropical Cyclones in the Eastern Pacific
    P2H.8 LANDFALLING TROPICAL CYCLONES IN THE EASTERN PACIFIC. PART I: CASE STUDIES FROM 2006 AND 2007. Luis M. Farfán1, Rosario Romero-Centeno2, G. B. Raga2 and Jorge Zavala-Hidalgo2 1Unidad La Paz, CICESE, Mexico 2Centro de Ciencias de la Atmósfera, Universidad Nacional Autónoma de México, Mexico 1. INTRODUCTION Western Mexico routinely experiences landfall of those that moved onto the mainland acquired a significant tropical cyclones. Jáuregui (2003) documented that 65 eastward component by 20ºN. Additionally, most storms hurricanes approached the west coast and 60% of them developed late in the season with highest frequency made landfall in the northwestern part of the country during the last two-thirds of September (35%) and all of between 1951 and 2000. This area is located north of October (54%). In a study of the period 1966-2004, 20ºN and west of 105ºW, which includes the Baja Romero-Vadillo et al. (2007) identified this type of storm California Peninsula and the States of Nayarit, Sinaloa track and the landfall trend associated with the presence and Sonora. Also, 64% of 88 tropical storms entered this of westerly airflow at middle and upper levels. area, increasing precipitation in this very arid region. Some of these systems continued moving northward after landfall and, eventually, had an influence on the weather conditions in the southwestern United States. The records for the eastern Pacific basin, provided by the National Hurricane Center, reveal 614 tropical cyclones during 1970–2007. Figure 1 displays the tracks of the sub-group of tropical cyclones that made landfall over northwestern Mexico. The upper panel (Fig.
    [Show full text]
  • Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific Ab Sins Nicholas S
    Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School March 2019 Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific aB sins Nicholas S. Grondin Louisiana State University, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Climate Commons, Meteorology Commons, and the Physical and Environmental Geography Commons Recommended Citation Grondin, Nicholas S., "Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific asinB s" (2019). LSU Master's Theses. 4864. https://digitalcommons.lsu.edu/gradschool_theses/4864 This Thesis is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Master's Theses by an authorized graduate school editor of LSU Digital Commons. For more information, please contact [email protected]. CLIMATOLOGY, VARIABILITY, AND RETURN PERIODS OF TROPICAL CYCLONE STRIKES IN THE NORTHEASTERN AND CENTRAL PACIFIC BASINS A Thesis Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Master of Science in The Department of Geography and Anthropology by Nicholas S. Grondin B.S. Meteorology, University of South Alabama, 2016 May 2019 Dedication This thesis is dedicated to my family, especially mom, Mim and Pop, for their love and encouragement every step of the way. This thesis is dedicated to my friends and fraternity brothers, especially Dillon, Sarah, Clay, and Courtney, for their friendship and support. This thesis is dedicated to all of my teachers and college professors, especially Mrs.
    [Show full text]
  • 2017 Dean's Report
    PARDEE RAND DEAN’S REPORT GRADUATE 2017 SCHOOL REPORT TO THE BOARD OF GOVERNORS SUSAN L. MARQUIS, DEAN YEAR IN REVIEW Message from the Dean NNOVATION.” In our research. In our tools and methods. In our systems and processes. In the development and application of technology. We’re not talking about a buzzword here. We’re talking about doing things better. Asking different questions. Turning things around. Not resting on “Iour laurels but looking for new ways to solve problems that no one has solved before. This is innovation at RAND—and it’s essential for RAND to remain relevant and influential in the 21st century. It’s what our clients, policymakers, and our communities need and demand. When RAND’s president and CEO Michael Rich talks about his SUSAN L. MARQUIS, DEAN vision for RAND and for the Pardee RAND Graduate School, he speaks about the school as a competitive advantage for RAND—a secret weapon that should be a primary engine of With this world- innovation for RAND. When Michael asked me, the dean, to take on the additional role of vice president for innovation, he was class graduate school asking Pardee RAND to not only aspire to but to fully claim this within this world-class unique role of strengthening the environment for innovation across all of RAND. With this world-class graduate school within research organization, this world-class research organization, both institutions can provide more—and accomplish more—than other research and both institutions can policy organizations. provide more—and For the past few years, you’ve heard us talk about “reimagining Pardee RAND.” The imperatives for change for the school and accomplish more— RAND are powerful.
    [Show full text]
  • Entidad Municipio Localidad Long
    Entidad Municipio Localidad Long Lat Durango Canelas EL PUERTO DEL AGUA 1062914 250413 Durango Canelas LA ESPERANZA 1062624 250517 Durango Canelas TIERRA AZUL 1063131 250513 Durango Tamazula ACACHUANE 1065724 250032 Durango Tamazula ACATITA GRANDE (ACATITA) 1070241 245957 Durango Tamazula ACATITÁN 1065314 245515 Durango Tamazula AGUA CALIENTE 1065409 245957 Durango Tamazula AMACUABLE 1065346 250120 Durango Tamazula ARROYO GRANDE DE MATAVACAS 1064810 245810 Durango Tamazula ARROYO SECO 1070229 250917 Durango Tamazula ARROYO VERDE (LOS TOROS) 1070501 251322 Durango Tamazula BOCA DE ARROYO DEL ZAPOTE 1070928 251937 Durango Tamazula CARRICITOS 1064943 245009 Durango Tamazula CARRICITOS 1070249 251420 Durango Tamazula CHACALA 1064419 244842 Durango Tamazula CHACOAL 1065650 250231 Durango Tamazula CHAPOTÁN 1065205 245646 Durango Tamazula COLOMA 1065530 245655 Durango Tamazula COLOMITA 1065621 245546 Durango Tamazula EL AGUAJE 1065350 245840 Durango Tamazula EL ARRAYANAL 1064818 250134 Durango Tamazula EL AYALI 1070620 251752 Durango Tamazula EL BARCO 1070521 251743 Durango Tamazula EL BLEDAL 1065306 250318 Durango Tamazula EL CARRIZAL 1065546 245836 Durango Tamazula EL CASTILLO 1065638 245802 Durango Tamazula EL CHILAR 1065806 251056 Durango Tamazula EL FILTRO 1070118 250911 Durango Tamazula EL FRIJOLAR 1065030 250228 Durango Tamazula EL GACHUPÍN 1065149 245910 Durango Tamazula EL GALERÓN 1070501 251506 Durango Tamazula EL GATO 1065744 251410 Durango Tamazula EL GUAMUCHILAR 1070548 251742 Durango Tamazula EL GUAMUCHILITO 1064542 244741 Durango
    [Show full text]
  • Extension of the Systematic Approach to Tropical Cyclone Track Forecasting in the Eastern and Central North Pacific
    NPS ARCHIVE 1997.12 BOOTHE, M. NAVAL POSTGRADUATE SCHOOL Monterey, California THESIS EXTENSION OF THE SYTEMATIC APPROACH TO TROPICAL CYCLONE TRACK FORECASTING IN THE EASTERN AND CENTRAL NORTH PACIFIC by Mark A. Boothe December, 1997 Thesis Co-Advisors: Russell L.Elsberry Lester E. Carr III Thesis B71245 Approved for public release; distribution is unlimited. DUDLEY KNOX LIBRARY NAVAl OSTGRADUATE SCHOOL MONTEREY CA 93943-5101 REPORT DOCUMENTATION PAGE Form Approved OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instruction, searching casting data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Washington Headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302, and to the Office of Management and Budget, I'aperwork Reduction Project (0704-0188) Washington DC 20503. 1 . AGENCY USE ONLY (Leave blank) 2. REPORT DATE 3. REPORT TYPE AND DATES COVERED December 1997. Master's Thesis TITLE AND SUBTITLE EXTENSION OF THE SYSTEMATIC 5. FUNDING NUMBERS APPROACH TO TROPICAL CYCLONE TRACK FORECASTING IN THE EASTERN AND CENTRAL NORTH PACIFIC 6. AUTHOR(S) Mark A. Boothe 7. PERFORMING ORGANIZATION NAME(S) AND ADDR£SS(ES) PERFORMING Naval Postgraduate School ORGANIZATION Monterey CA 93943-5000 REPORT NUMBER 9. SPONSORING/MONITORING AGENCY NAME(S) AND ADDRESSEES) 10. SPONSORING/MONTTORIN G AGENCY REPORT NUMBER 11. SUPPLEMENTARY NOTES The views expressed in this thesis are those of the author and do not reflect the official policy or position of the Department of Defense or the U.S.
    [Show full text]
  • UCLA Electronic Theses and Dissertations
    UCLA UCLA Electronic Theses and Dissertations Title The Indifferent Subnational State: Sinaloan State Government relations with its Diaspora in Los Angeles Permalink https://escholarship.org/uc/item/7t329901 Author VILLEGAS RIVERA, FERNANDO ENRIQUE Publication Date 2019 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California UNIVERSITY OF CALIFORNIA Los Angeles The Indifferent Subnational State: Sinaloan State Government relations with its Diaspora in Los Angeles A thesis submitted in partial satisfaction of the requirements for the degree Masters of Arts in Chicana and Chicano Studies by Fernando Enrique Villegas Rivera 2019 © Copyright by Fernando Enrique Villegas Rivera 2019 ABSTRACT OF THE THESIS The Indifferent Subnational State: Sinaloan State Government relations with its Diaspora in Los Angeles by Fernando Enrique Villegas Rivera Master of Arts in Chicana and Chicano Studies University of California, Los Angeles, 2019 Professor Matthew Alejandro Barreto, Chair The Mexican state of Sinaloa has not developed diaspora policies directed to the Sinaloan Diaspora in the United States, even though the economic and social contributions to the state are significant and despite the existence of a significant group of Sinaloans in a situation of extreme vulnerability due to their precarious legal status. Current literature on diaspora policies has not developed a framework to understand atypical cases such as the case of Sinaloa. I developed a mixed method research design case study of state-diaspora relations in the Sinaloa-Los Angeles transnational field. I argue that political, economic, and organizational factors explain the absence of diaspora policies. Findings suggest that this is due to anti-democratic orientations of Sinaloan local governments, lack of strong Sinaloan Hometown Associations, and low remittance dependency at the state level.
    [Show full text]
  • Notable Tropical Cyclones and Unusual Areas of Tropical Cyclone Formation
    A flood is an overflow of an expanse of water that submerges land.[1] The EU Floods directive defines a flood as a temporary covering by water of land not normally covered by water.[2] In the sense of "flowing water", the word may also be applied to the inflow of the tide. Flooding may result from the volume of water within a body of water, such as a river or lake, which overflows or breaks levees, with the result that some of the water escapes its usual boundaries.[3] While the size of a lake or other body of water will vary with seasonal changes in precipitation and snow melt, it is not a significant flood unless such escapes of water endanger land areas used by man like a village, city or other inhabited area. Floods can also occur in rivers, when flow exceeds the capacity of the river channel, particularly at bends or meanders. Floods often cause damage to homes and businesses if they are placed in natural flood plains of rivers. While flood damage can be virtually eliminated by moving away from rivers and other bodies of water, since time out of mind, people have lived and worked by the water to seek sustenance and capitalize on the gains of cheap and easy travel and commerce by being near water. That humans continue to inhabit areas threatened by flood damage is evidence that the perceived value of living near the water exceeds the cost of repeated periodic flooding. The word "flood" comes from the Old English flod, a word common to Germanic languages (compare German Flut, Dutch vloed from the same root as is seen in flow, float; also compare with Latin fluctus, flumen).
    [Show full text]
  • MASARYK UNIVERSITY BRNO Diploma Thesis
    MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION DEPARTMENT OF ENGLISH LANGUAGE AND LITERATURE Presentation Sentences in Wikipedia: FSP Analysis Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský Declaration I declare that I have worked on this thesis independently, using only the primary and secondary sources listed in the bibliography. I agree with the placing of this thesis in the library of the Faculty of Education at the Masaryk University and with the access for academic purposes. Brno, 30th March 2018 …………………………………………. Bc. Lukáš Opavský Acknowledgements I would like to thank my supervisor, doc. Mgr. Martin Adam, Ph.D. for his kind help and constant guidance throughout my work. Bc. Lukáš Opavský OPAVSKÝ, Lukáš. Presentation Sentences in Wikipedia: FSP Analysis; Diploma Thesis. Brno: Masaryk University, Faculty of Education, English Language and Literature Department, 2018. XX p. Supervisor: doc. Mgr. Martin Adam, Ph.D. Annotation The purpose of this thesis is an analysis of a corpus comprising of opening sentences of articles collected from the online encyclopaedia Wikipedia. Four different quality categories from Wikipedia were chosen, from the total amount of eight, to ensure gathering of a representative sample, for each category there are fifty sentences, the total amount of the sentences altogether is, therefore, two hundred. The sentences will be analysed according to the Firabsian theory of functional sentence perspective in order to discriminate differences both between the quality categories and also within the categories.
    [Show full text]
  • Yu-Feng Hsu and Jerry A. Powell
    Phylogenetic Relationships within Heliodinidae and Systematics of Moths Formerly Assigned to Heliodines Stainton (Lepidoptera: Yponomeutoidea) Yu-Feng Hsu and Jerry A. Powell Phylogenetic Relationships within Heliodinidae and Systematics of Moths Formerly Assigned to Heliodines Stainton (Lepidoptera: Yponomeutoidea) Yu-Feng Hsu and Jerry A. Powell UNIVERSITY OF CALIFORNIA PRESS Berkeley • Los Angeles • London UNIVERSITY OF CALIFORNIA PUBLICATIONS IN ENTOMOLGY Editorial Board: Penny Gullan, Bradford A. Hawkins, John Heraty, Lynn S. Kimsey, Serguei V. Triapitsyn, Philip S. Ward, Kipling Will Volume 124 UNIVERSITY OF CALIFORNIA PRESS BERKELEY AND LOS ANGELES, CALIFORNIA UNIVERSITY OF CALIFORNIA PRESS, LTD. LONDON, ENGLAND © 2005 BY THE REGENTS OF THE UNIVERSITY OF CALIFORNIA PRINTED IN THE UNITED STATES OF AMERICA Library of Congress Cataloging-in-Publication Data Hsu, Yu-Feng, 1963– Phylogenetic relationships within Heliodinidae and systematics of moths formerly assigned to Heliodines Stainton (Lepidoptera: Yponomeutoidea) / Yu-Feng Hsu and Jerry A. Powell. p. cm. Includes bibliographical references. ISBN 0-520-09847-1 (paper : alk. paper) — (University of California publications in entomology ; 124) 1. Heliodinidae—Classification. 2. Heliodinidae—Phylogeny. I. Title. II. Series. QL561.H44 H78 595.78 22—dc22 2004058800 Manufactured in the United States of America The paper used in this publication meets the minimum requirements of ANSI/NISO Z39.48-1992 (R 1997) (Permanence of Paper). Contents Acknowledgments, ix Abstract, xi Introduction ...................................................... 1 Problems in Systematics of Heliodinidae and a Historical Review ............ 4 Material and Methods ............................................ 6 Specimens and Depositories, 6 Dissections and Measurements, 7 Wing Venation Preparation, 7 Scanning Electron Microscope Preparation, 8 Species Discrimination and Description, 8 Larval Rearing Procedures, 8 Phylogenetic Methods, 9 Phylogeny of Heliodinidae ........................................
    [Show full text]
  • 81236 Sinaloa 7125001 Ahome 10 De Mayo 81271 Sinaloa 7125001 Ahome 12 De Octubre 81360 Sinaloa 7125001 Ahome 18 De Marzo 81363 S
    81236 SINALOA 7125001 AHOME 10 DE MAYO 81271 SINALOA 7125001 AHOME 12 DE OCTUBRE 81360 SINALOA 7125001 AHOME 18 DE MARZO 81363 SINALOA 7125001 AHOME 20 DE NOVIEMBRE NUEVO 81363 SINALOA 7125001 AHOME 20 DE NOVIEMBRE VIEJO 81375 SINALOA 7125001 AHOME 24 DE FEBRERO 81238 SINALOA 7125001 AHOME 28 DE JUNIO 81361 SINALOA 7125001 AHOME 5 DE MAYO 81234 SINALOA 7125001 AHOME 75 (HERIBERTO VALDEZ ROMERO) 81379 SINALOA 7125001 AHOME 9 DE DICIEMBRE 81238 SINALOA 7125001 AHOME ADOLFO LOPEZ MATEOS 81372 SINALOA 7125001 AHOME ADUANA 81303 SINALOA 7125001 AHOME AGUA NUEVA 81307 SINALOA 7125001 AHOME AGUILA AZTECA 81315 SINALOA 7125001 AHOME AHOME CENTRO 81318 SINALOA 7125001 AHOME AHOME INDEPENDENCIA 81318 SINALOA 7125001 AHOME AHOME INDEPENDIENTE 81248 SINALOA 7125001 AHOME ALAMO 81248 SINALOA 7125001 AHOME ALAMOS 81271 SINALOA 7125001 AHOME ALAMOS COUNTRY 81248 SINALOA 7125001 AHOME ALAMOS I 81248 SINALOA 7125001 AHOME ALAMOS II 81367 SINALOA 7125001 AHOME ALBERGUE LOUISIANA 81278 SINALOA 7125001 AHOME ALCAZAR DEL COUNTRY 81260 SINALOA 7125001 AHOME ALEJANDRO PEÑA 81236 SINALOA 7125001 AHOME ALFONSO G CALDERON 81346 SINALOA 7125001 AHOME ALFONSO G. CALDERON (POBLADO SIETE) 81240 SINALOA 7125001 AHOME ALFREDO SALAZAR 81240 SINALOA 7125001 AHOME ALMA GUADALUPE ESTRADA 81294 SINALOA 7125001 AHOME ALMENDRAS 81289 SINALOA 7125001 AHOME AMERICANA 81290 SINALOA 7125001 AHOME AMPLIACION BUROCRATA 81294 SINALOA 7125001 AHOME AMPLIACION NUEVO SIGLO 81280 SINALOA 7125001 AHOME ANAHUAC 81320 SINALOA 7125001 AHOME ANTONIO TOLEDO CORRO 81285 SINALOA 7125001 AHOME
    [Show full text]
  • P2h.8 Landfalling Tropical Cyclones in the Eastern Pacific
    P2H.8 LANDFALLING TROPICAL CYCLONES IN THE EASTERN PACIFIC. PART I: CASE STUDIES FROM 2006 AND 2007. Luis M. Farfán1, Rosario Romero-Centeno2, G. B. Raga2 and Jorge Zavala-Hidalgo2 1Unidad La Paz, CICESE, Mexico 2Centro de Ciencias de la Atmósfera, Universidad Nacional Autónoma de México, Mexico 1. INTRODUCTION Western Mexico routinely experiences landfall of those that moved onto the mainland acquired a significant tropical cyclones. Jáuregui (2003) documented that 65 eastward component by 20ºN. Additionally, most storms hurricanes approached the west coast and 60% of them developed late in the season with highest frequency made landfall in the northwestern part of the country during the last two-thirds of September (35%) and all of between 1951 and 2000. This area is located north of October (54%). In a study of the period 1966-2004, 20ºN and west of 105ºW, which includes the Baja Romero-Vadillo et al. (2007) identified this type of storm California Peninsula and the States of Nayarit, Sinaloa track and the landfall trend associated with the presence and Sonora. Also, 64% of 88 tropical storms entered this of westerly airflow at middle and upper levels. area, increasing precipitation in this very arid region. Some of these systems continued moving northward after landfall and, eventually, had an influence on the weather conditions in the southwestern United States. The records for the eastern Pacific basin, provided by the National Hurricane Center, reveal 614 tropical cyclones during 1970–2007. Figure 1 displays the tracks of the sub-group of tropical cyclones that made landfall over northwestern Mexico. The upper panel (Fig.
    [Show full text]
  • Proceedings of the Twenty-Eighth Annual Symposium on Sea Turtle Biology and Conservation
    NOAA Technical Memorandum NMFS-SEFSC-602 PROCEEDINGS OF THE TWENTY-EIGHTH ANNUAL SYMPOSIUM ON SEA TURTLE BIOLOGY AND CONSERVATION 22 to 26 January 2008 Loreto, Baja California Sur, México Compiled by: Kama Dean & Melania C. López Castro U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Marine Fisheries Service Southeast Fisheries Science Center 75 Virginia Beach Drive Miami, Florida 33149 March 2010 NOAA Technical Memorandum NMFS-SEFSC-602 PROCEEDINGS OF THE TWENTY-EIGHTH ANNUAL SYMPOSIUM ON SEA TURTLE BIOLOGY AND CONSERVATION 22 to 26 January 2008 Loreto, Baja California Sur, México Compiled by: Kama Dean & Melania C. López Castro U.S. DEPARTMENT OF COMMERCE Gary Locke, Secretary NATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION Dr. Jane Lubchenco, Under Secretary for Oceans and Atmosphere NATIONAL MARINE FISHERIES SERVICE Eric C. Schwaab, Assistant Administrator for Fisheries March 2010 This Technical Memorandum series is used for documentation and timely communication of preliminary results, interim reports, or similar special-purpose information. Although the memoranda are not subject to complete formal review, editorial control or detailed editing, they are expected to reflect sound professional work. NOTICE The National Marine Fisheries Service (NMFS) does not approve, recommend or endorse any proprietary product or material mentioned in this publication. No references shall be made to NMFS, or to this publication furnished by NMFS, in any advertising or sales promotion which would imply that NMFS approves, recommends or endorses any proprietary product or proprietary material herein which has as its purpose any intent to cause directly or indirectly the advertised product to be use or purchased because of NMFS publication.
    [Show full text]