Nubes Y Fenómenos Nubes Bajas Figura 1 – Stratocumulus Stratiformis Opacus Undulatus Figura 2 – Stratocumulus Stratiformis

Total Page:16

File Type:pdf, Size:1020Kb

Nubes Y Fenómenos Nubes Bajas Figura 1 – Stratocumulus Stratiformis Opacus Undulatus Figura 2 – Stratocumulus Stratiformis Nubes y Fenómenos Nubes bajas Figura 1 – Stratocumulus Stratiformis Opacus Undulatus Figura 2 – Stratocumulus Stratiformis Traslucidus Nubes bajas Figura 3 – Stratocumulus Stratiformis Traslucidus Perlucidus Figura 4 – Stratus Nebulosus Undulatus 2 Nubes bajas Figura 5 – Stratus , Fractostratus y Fractocumulus bajo Altostratus Figura 6 – Cumulus humilis 3 Nubes bajas Figura 7 – Cumulus mediocris Figura 8 – Cumulus Cumulugenitus 4 Nubes bajas Figura 9 – Cumulunimbus Calvus Figura 10 – Cumulunimbus Capillatus Mediocris y Congestus 5 Nubes bajas Figura 11 – Cumulunimbus Calvus con ráfagas Figura 12 – Cumulunimbus Capillatus Incus 6 Nubes bajas Figura 13 – Cumulunimbus con Arcus Figura 14 – Mammatus 7 Nubes medias Figura 15 – Altostratus Traslucidus Figura 16 – Altostratus y Fractocumulus 8 Nubes medias Figura 17 – Nimbustratus Figura 18 – Nimbustratus y Fractostratus 9 Nubes medias Figura 19 – Altocumulus Traslucidus Figura 20 – Altocumulus Stratiformis Traslucidus Perlucidus 10 Nubes medias Figura 21 – Altocumulus Stratiformis Perlucidus Undulatus Figura 22 – Altocumulus Stratiformis Traslucidus Undulatus 11 Nubes medias Figura 23– Altocumulus Stratiformis Opacus Figura 24– Altocumulus Cumulugenitus 12 Nubes medias Figura 25– Altocumulus Castellanus Figura 26– Altocumulus Floccus 13 Nubes medias Figura 27– Altocumulus Lenticularis Figura 28– Altocumulus Lenticularis 14 Nubes medias Figura 29– Altocumulus Lenticularis Duplicatus Figura 30 – Altostratus Traslucidus y Altocumulus Stratiformis 15 Nubes medias Figura 31 – Altostratus Undulatus Radiatus Traslucidus Figura 32 – Altocumulus Castellanus y Cumulus Congestus 16 Nubes medias Figura 33– Cielo Caótico Figura 34– Cielo Caótico 17 Nubes altas Figura 35– Cirrus uncinus Figura 36– Cirrus uncinus y fibratus 18 Nubes altas Figura 37– Cirrus uncinus radiatus Figura 38– Cirrus Fibratus 19 Nubes altas Figura 39– Cirrus Fibratus Vertebratus Figura 40– Cirrus Fibratus y Cirrostratus 20 Nubes altas Figura 41– Cirrus Traslucidus Fibratus Figura 42– Cirrus Spissatus y Cumulunimbus 21 Nubes altas Figura 43 – Cirrus, Cirrostratus y Altocumulus Figura 44 – Cirrus Spissatus con Virga 22 Nubes altas Figura 45– Cirrus Floccus Figura 46 – Cirrus Floccus con virga y Cirrocumulus floccus 23 Nubes altas Figura 47– Cirrocumulus Stratiformis Undulatus Figura 48– Cirrocumulus Stratiformis Undulatus Lacunosus 24 Nubes orográficas Figura 49– Muro de Föhn Figura 50 – Altocumulus y Altostratus orográficos 25 Nubes Especiales Figura 51 – Nube nacarada Figura 52 – Nubes Noctilucentes 26 Nubes Especiales Figura 53 – Estelas de Condensación Fenómenos Figura 54 – Niebla densa sobre superficie de agua 27 Fenómenos Figura 55 – Niebla densa en bancos Figura 56 – Niebla y humo (SMOG) 28 Fenómenos Figura 57 – Niebla de radiación Figura 58– Niebla y Stratus en valle de montaña 29 Fenómenos Figura 59 – Chaparrón de nieve Figura 60 – Gránulos de nieve 30 Fenómenos Figura 61 – Granizo Figura 62 – Spray 31 Fenómenos Figura 63 – Cencellada Figura 64 – Cencellada 32 Fenómenos Figura 65 – Tromba Figura 66 – Tornado 33 Fenómenos Figura 67 – Torbellino de polvo Figura 68 – Halo 34 Fenómenos Figura 69 – Arco Iris y Chaparrón de lluvia Figura 70 – Rayo 35 Fenómenos Figura 71 – Rayos de Sol crepusculares Figura 72– Rayos de Sol crepusculares 36 Fenómenos Figura 73 – Irisación Figura 74 – Aurora Polar 37 .
Recommended publications
  • New Cloud Types 2019
    UPSC MAIN & PRELIMS NEW CLOUD TYPES 2019 BY : NEETU SINGH This is updated material for New Cloud Types, targeting both upcoming Prelims and Main Exams. Video is attached to provide you with the gist of content. https://youtu.be/01Ciwd9b470 New Cloud Types PRINCIPLES OF CLOUD CLASSIFICATION Useful concepts Height, altitude, vertical extent Clouds continuously evolve and appear in an infinite variety of forms. However, there is a limited number · Height: Vertical distance from the point of of characteristic forms frequently observed all over observation on the Earth's surface to the point the world, into which clouds can be broadly grouped being measured. in a classification scheme. The scheme uses · Altitude: Vertical distance from mean sea level to genera(defined according to their appearance and the point being measured. position in the sky), species(describing shape and · Height/Altitude of cloud base: For surface structure) and varieties(describing transparency and observations, height of the cloud base above arrangement).This is similar to the systems used in ground level; for aircraft observations, altitude of the classification of plants or animals, and similarly the cloud base above mean sea level. uses Latin names. · Vertical extent: Vertical distance from a cloud's There are some intermediate or transitional forms of base to its top. clouds that, although observed fairly frequently, are Levels not described in the classification scheme. The transitional forms are of little interest; they are less Clouds are generally encountered over a range of stable and in appearance are not very different from altitudes varying from sea level to the top of the the definitions of the characteristic forms.
    [Show full text]
  • ICA Vol. 1 (1956 Edition)
    ·wMo o '-" I q Sb 10 c. v. i. J c.. A INTERNATIONAL CLOUD ATLAS Volume I WORLD METEOROLOGICAL ORGANIZATION 1956 c....._/ O,-/ - 1~ L ) I TABLE OF CONTENTS Pages Preface to the 1939 edition . IX Preface to the present edition . xv PART I - CLOUDS CHAPTER I Introduction 1. Definition of a cloud . 3 2. Appearance of clouds . 3 (1) Luminance . 3 (2) Colour .... 4 3. Classification of clouds 5 (1) Genera . 5 (2) Species . 5 (3) Varieties . 5 ( 4) Supplementary features and accessory clouds 6 (5) Mother-clouds . 6 4. Table of classification of clouds . 7 5. Table of abbreviations and symbols of clouds . 8 CHAPTER II Definitions I. Some useful concepts . 9 (1) Height, altitude, vertical extent 9 (2) Etages .... .... 9 2. Observational conditions to which definitions of clouds apply. 10 3. Definitions of clouds 10 (1) Genera . 10 (2) Species . 11 (3) Varieties 14 (4) Supplementary features and accessory clouds 16 CHAPTER III Descriptions of clouds 1. Cirrus . .. 19 2. Cirrocumulus . 21 3. Cirrostratus 23 4. Altocumulus . 25 5. Altostratus . 28 6. Nimbostratus . 30 " IV TABLE OF CONTENTS Pages 7. Stratoculllulus 32 8. Stratus 35 9. Culllulus . 37 10. Culllulonimbus 40 CHAPTER IV Orographic influences 1. Occurrence, structure and shapes of orographic clouds . 43 2. Changes in the shape and structure of clouds due to orographic influences 44 CHAPTER V Clouds as seen from aircraft 1. Special problellls involved . 45 (1) Differences between the observation of clouds frolll aircraft and frolll the earth's surface . 45 (2) Field of vision . 45 (3) Appearance of clouds. 45 (4) Icing .
    [Show full text]
  • The Ten Different Types of Clouds
    THE COMPLETE GUIDE TO THE TEN DIFFERENT TYPES OF CLOUDS AND HOW TO IDENTIFY THEM Dedicated to those who are passionately curious, keep their heads in the clouds, and keep their eyes on the skies. And to Luke Howard, the father of cloud classification. 4 Infographic 5 Introduction 12 Cirrus 18 Cirrocumulus 25 Cirrostratus 31 Altocumulus 38 Altostratus 45 Nimbostratus TABLE OF CONTENTS TABLE 51 Cumulonimbus 57 Cumulus 64 Stratus 71 Stratocumulus 79 Our Mission 80 Extras Cloud Types: An Infographic 4 An Introduction to the 10 Different An Introduction to the 10 Different Types of Clouds Types of Clouds ⛅ Clouds are the equivalent of an ever-evolving painting in the sky. They have the ability to make for magnificent sunrises and spectacular sunsets. We’re surrounded by clouds almost every day of our lives. Let’s take the time and learn a little bit more about them! The following information is presented to you as a comprehensive guide to the ten different types of clouds and how to idenify them. Let’s just say it’s an instruction manual to the sky. Here you’ll learn about the ten different cloud types: their characteristics, how they differentiate from the other cloud types, and much more. So three cheers to you for starting on your cloud identification journey. Happy cloudspotting, friends! The Three High Level Clouds Cirrus (Ci) Cirrocumulus (Cc) Cirrostratus (Cs) High, wispy streaks High-altitude cloudlets Pale, veil-like layer High-altitude, thin, and wispy cloud High-altitude, thin, and wispy cloud streaks made of ice crystals streaks
    [Show full text]
  • An Introduction to Clouds
    Clouds National Meteorological Library and Archive Fact sheet 1 — An introduction to clouds The National Meteorological Library and Archive Many people have an interest in the weather and the processes that cause it, which is why the National Meteorological Library and Archive are open to everyone. Holding one of the most comprehensive collections on meteorology anywhere in the world, the Library and Archive are vital for the maintenance of the public memory of the weather, the storage of meteorological records and as aid of learning. The Library and Archive collections include: • around 300,000 books, charts, atlases, journals, articles, microfiche and scientific papers on meteorology and climatology, for a variety of knowledge levels • audio-visual material including digitised images, slides, photographs, videos and DVDs • daily weather reports for the United Kingdom from 1861 to the present, and from around the world • marine weather log books • a number of the earliest weather diaries dating back to the late 18th century • artefacts, records and charts of historical interest; for example, a chart detailing the weather conditions for the D-Day Landings, the weather records of Scott’s Antarctic expedition from 1911 • rare books, including a 16th century edition of Aristotle’s Meteorologica, held on behalf of the Royal Meteorological Society • a display of meteorological equipment and artefacts For more information about the Library and Archive please see our website at: www.metoffice.gov.uk/learning/library Introduction A cloud is an aggregate of very small water droplets, ice crystals, or a mixture of both, with its base above the Earth’s surface.
    [Show full text]
  • Cloud Types for Observers Reading the Sky
    Cloud types for observers Reading the sky Cloud types for observers Reading the sky Cloud types for obser vers 1 Introduction Clouds are continually changing and appear in an infinite The descriptions and photographs which follow are given variety of forms. It is possible, however, to define a limited in the same order as the code figures in the pictorial guide. number of characteristic forms observed all over the world To find the correct code figure from the pictorial guides, into which clouds can be broadly grouped. The World start at whichever circle is applicable at the top of the page Meteorological Organization (WMO) has drawn up a and follow the solid line from description to description as classification of these characteristic forms to enable an long as all the criteria are applicable. If a description is observer to report the types of cloud present. This reached which is not applicable, return to the previous publication illustrates and explains the classifications. description and take the pecked line to a picture square. The correct code figure will be found in the top right­hand Classification is based on 10 main groups of clouds. These corner of the picture square. are divided into three levels — low, medium and high — according to that part of the atmosphere in which they are Distinguishing features connected with the 10 main groups usually found. A code figure designated CL, CM or CH is of clouds are listed at the end of this publication. Observers used to describe the clouds of each level. The divisions are may find this a useful guide when considering which shown in the table below.
    [Show full text]
  • Atmospheric Moisture, Air Masses & Fronts By: Neetu Singh
    ATMOSPHERIC MOISTURE, AIR MASSES & FRONTS BY: NEETU SINGH Atmospheric Moisture The fourth element of weather and climate is moisture. This might seem a familiar feature because everyone knows what water is. In actuality, however, most atmospheric moisture occurs not as liquid water but rather as water vapour, which is much less conspicuous and much less familiar. One of the most distinctive attributes of water is that it occurs in the atmosphere in three physical states – solid (snow, hail, sleet, and ice), liquid (rain, water droplets) and gas (water vapour). Of the three states, the gas state is the most important insofar as the dynamics of the atmosphere are concerned. The impact of Atmospheric Moisture on the Landscape When the atmosphere contains enough moisture, water vapour may condense to form haze, fog, cloud, rain, sleet, hail, or snow, producing a skyscape that is both visible and tangible. Precipitation produces dramatic short-run changes in the landscape whenever rain puddles form, streams and rivers flood, or snow and ice blanket the ground. The long-term effect of atmospheric moisture is even more fundamental. Water vapour stores energy that can galvanize the atmosphere into action, as, for example, in the way rainfall and snowmelt in soil and rock are an integral part of weathering and erosion. In addition, the presence or absence of precipitation is critical to the survival of almost all forms of terrestrial vegetation. Water Vapour and the Hydrologic Cycle Water vapour is a colourless, odourless, tasteless, invisible gas that mixes freely with the other gases of the atmosphere. We are likely to become aware of water vapour when humidity is high because the air feels sticky, clothes feel damp, and our skin feels clammy, or when humidity is low because our lips chap and our hair will not behave.
    [Show full text]
  • Wispy Alejandra Abad Cloud Report Class: Flow Visualization - ARTF 5200-001 ​ Date: 10/28/19
    Wispy Alejandra Abad Cloud Report Class: Flow Visualization - ARTF 5200-001 ​ Date: 10/28/19 Cirrus Cloud I thought my image was a Cirrus Uncinus at first. I had come to this conclusion because these are the type of clouds that tend to have curls. Cirrus clouds are known as "mare's tails" which I found interesting. In this photo I wanted to explore why this cloud was at an angle and creating wispy trails. After I did some research it looked like this photo was the trail of a Cirrus floccus formed over ​ time by cirrostratus clouds below. According to UCAR ​ ​ Center for Science Education, “Cirrus clouds are often ​ ​ seen during fair weather. But if they build up larger over time and are followed by cirrostratus clouds, there may be a warm front on the way.” This cloud description makes far more sense to the phenomena I experienced that day. On October 9th, I took the picture shown to the right. It was taken at 6pm, across from the Libby Hall on campus. I faced north towards the stadium and I pointed up at an angle using a telephoto lens. Cirrus clouds are seen at high altitudes in the troposphere and again at higher points. The parcel is cooler and the ceilometer says the clouds where anywhere from 5 – 6 kilometers up high. Cirrus clouds can form at any altitude between 16,500 ft (5.0 km; 3.13 mi) and 45,000 ​ ft (14 km; 8.5 mi) above sea level. (Cirrus Cloud, 2019). ​ ​ ​ ​ ​ In the photograph you can’t see the cirrostratus clouds below however I believe that the ​ phenomena is due to the crystal ice cloud, Cirrus floccus that formed from cirrostratus clouds.
    [Show full text]
  • Observación E Identificación De Nubes
    OBSERVACIÓN E IDENTIFICACIÓN DE NUBES Francisco Martín León José Antonio Quirantes AGRADECIMIENTOS Los autores quieren dar las gracias a Carlos García Legaz y Carlos Almarza, ambos del INM, así como a Josep Enric Llebot del Departament de Física de la Universitat Autònoma de Barcelona por sus comentarios y sugerencias que han servido para enriquecer esta Unidad. OBJETIVO DE LA UNIDAD 94 1. INTRODUCCIÓN 96 1.1. La nube como un eslabón del ciclo del agua 97 1.2. Mecanismos de ascensos de masas de aire 99 Por qué es importante observar las nubes 100 2. CLASIFICACIÓN BÁSICA DE LAS NUBES 108 a. Por su origen 108 b. Por su naturaleza 108 c. Por el nivel atmosférico que ocupan 109 d. Por sus formas 110 Tabla de las Clasificaciones nubosas 112 3. DESCRIPCIÓN DE LOS GÉNEROS DE NUBES: NUBES ESPECIALES 114 GÉNEROS DE NUBES, ABREVIATURAS Y SU SIGNIFICADO LATINO 115 4. AHORA TE TOCA A TI IDENTIFICARLAS 132 ANEXO I: CÓMO DOCUMENTAR LA FOTOGRAFÍA DE UNA NUBE 134 ANEXO II: TABLA DE CLASIFICACIÓN INTERNACIONAL DE LAS NUBES DE LA OMM 138 SOLUCIONES AL TEST DE FOTOGRAFÍAS DE NUBES: 140 Bibliografía 141 METEOROLOGÍA Y CLIMATOLOGÍA 93 UNIDAD DIDÁCTICA OBJETIVO DE LA UNIDAD Servir de elemento básico para la observación e identificación de las nubes desde la superficie terrestre. La unidad posee los elementos fundamentales para que los participantes del concurso de fotos “Cazadores de nubes” sean capaces de identificar cada género de nube fotografiada. Además, podrá ser usada como elemento de referencia en las tareas de observación meteorológica rutinarias y en las periódicas que se estime oportuno relacionada con otras actividades de observación habitual.
    [Show full text]
  • Special Clouds
    Special clouds Special clouds In addition, there are special cases where clouds may form or grow as a consequence of certain, often localized, generating factors. These may be either natural, or the result of human activity. Several cases of “special clouds” can be distinguished: Flammagenitus Clouds may develop as a consequence of convection Cumulus initiated by heat from forest fires, wildfires or volcanic eruption activity. Clouds that are clearly congestus observed to have originated as a consequence of flammagenitus localized natural heat sources, such as forest fires, wildfires or volcanic activity and which, at least in Cumulonimbus part, consist of water drops, will be given the name relevant to the genus followed, if appropriate, by calvus the species, variety and any supplementary flammagenitus features, and finally by the special cloud name “flammagenitus”. Cumulus flammagenitus is unofficially known as 'pyrocumulus' Homogenitus Clouds may also develop as a consequence of human activity. Examples are aircraft condensation trails (contrails), or clouds resulting from industrial Cumulus processes, such as cumuliform clouds generated by mediocris rising thermals above power station cooling towers. homogenitus Clouds that are clearly observed to have originated specifically as a consequence of human activity will be given the name of the appropriate genus, followed by the special cloud name “homogenitus”. For example, Cumulus cloud formed above industrial plants will be known as Cumulus (and, if appropriate, the species, variety and any supplementary features) followed by the special cloud name homogenitus; RTC-CN-008.3 Page 1 of 2 Aircraft Aircraft condensation trails (contrails) that have condensation persisted for at least 10 minutes will be given the name of the genus, Cirrus, followed only by the trails special cloud name “homogenitus”, so a contrail will be known only as Cirrus homogenitus.
    [Show full text]
  • Cloud Chart Photo Descriptions the Following Tables Provide Descriptions of the Clouds on the Cloud Identification Chart
    Cloud Chart Photo Descriptions The following tables provide descriptions of the clouds on the Cloud Identification Chart. The order of the descriptions matches the photos on the chart. The families appear here first followed by Accessory Clouds. High Family (above 16,500 ft/5,000 m) Genus species Genus Species Genus Species Genus Species Genus Species Genus Species Cirrus castellanus Cirrus fibratus Cirrus fibratus Cirrus floccus Cirrus spissatus Cirrus uncinus Cirrus – high, white, Cirrus - white, wispy, Cirrus - white, wispy, Cirrus - white, wispy, Cirrus - high, white, Cirrus - white, wispy, with hair like strands. feathery, hair like. feathery, hair like. feathery, hair like. with wispy edges. feathery, hair like. castellanus - castle fibratus – finely fibratus – finely floccus - tufts of spissatus - dense uncinus - white thin like towers. separated filaments. separated filaments. wool.rounded at the lumps that blot out the bands with hooked or top, ragged on the sun usually originating tufted top that is not Castle-like turrets Clouds with uniformly Clouds with uniformly bottom.. from the top of a rounded. rising from a common shaped fibers without shaped fibers without The streamers in this cumulonimbus. base. This cloud type distinctive hooks. They distinctive hooks. They photo are falling ice Sometimes the side Composed of ice is composed of ice are composed of ice are composed of ice crystals. Falling rain or away from the Sun is crystals. crystals and some crystals. crystals. snow that does not gray. super-cooled water reach the ground is Composed of ice droplets. called virga. crystals. Genus species Genus species Genus species Genus species Genus species Genus species Cirrrocumulus Cirrocumulus Cirrocumulus Cirrocumulus Cirrostratus fibratus Cirrostratus castellanus floccus lenticularis stratiformis nebulosus Cirro – of the High Cirro – of the High Cirro – of the High Cirro – of the High Cirro – of the High Cirro – of the High (Cirrus) Family.
    [Show full text]
  • Manual on the Observation of Clouds and Other Meteors
    WORLD METEOROLOGICAL ORGANIZATION INTERNATIONAL CL·OUD ATLAS Volume I Revised edition 1975 MANUAL ON THE OBSERVATION OF CLOUDS AND OTHER METEORS (Partly Annex I to WMO Technical Regulations) WMO - No. 407 Secretariat of the World Meteorological Organization - Geneva - Switzerland 1975 ( ( ( © 1975, World Meteorological Organization ISBN 92-63-10407-7 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. CONTENTS Pages Preface to the 1939 edition IX Preface to the 1956 edition xv Preface to the present edition XIX Introductory note ..... XXIII 1. PARTl DEFINITION OF A METEOR AND GENERAL CLASSIFICATION OF METEORS Ll Definition of a meteor .... 3 1.2 General classification of meteors 3 1.2.1 Hydrometeors 3 1.2.2 Lithometeors 5 1.2.3 Photometeors 5 1.2.4 Electrometeors 5 II.PARTII CLOUDS ILl INTRODUCTION 11.1.1 Definition of a cloud 9 II.1.2 Appearance of clouds 9 II.1.2.1 Luminance .... 9 II.1.2.2 Colour . 10 11.1.3 Principles of cloud classification 11 II.1.3.1 Genera. 11 II.1.3.2 Species .......... 11 II.1.3.3 Varieties ......... 11 II.1.3.4 Supplementary features and accessory clouds 12 II.1.3.5 Mother-clouds ....... 12 lLl.4 Table of classification of clouds 13 II.1.5 Table of abbreviations and symbols of clouds 14 11.2 DEFINITION OF CLOUDS II.2.1 Some useful concepts 15 11.2.1.1 Height, altitude, vertical extent 15 ( IV CONTENTS Pages 11.2.1.2 Etages .
    [Show full text]
  • 大气科学类词汇小词典made by Superjyq@Lilybbs 如有疏漏,敬请指正[A]
    大气科学类词汇小词典 Made by superjyq@lilybbs 如有疏漏,敬请指正 [A] a priori probability 先验机率 a priori reason 先验理由 A scope (indicator) A 示波器 Abbe number 阿贝数 ABC bucket ABC 吊桶 aberration 像差;光行差 aberwind 阿卑风 ablation 消冰;消冰量 ablation area 消冰区 abnormal 异常 abnormal lapse rate 异常直减率 abnormal propagation 异常传播 abnormal refraction 异常折射 abnormal weather 异常天气 abnormality 异常度;距平度 above normal 超常 Abraham's tree 亚伯拉罕树状卷云 abrego 阿勃列戈风 abroholos 亚伯落贺颮 Abrolhos squalls 亚伯落贺颮 abscissa 横坐标 absolute 绝对 absolute acceleration 绝对加速度 absolute altimeter 绝对高度计 absolute altitude 绝对高度 absolute angular momentum 绝对角动量 absolute annual range of temperature 温度绝对年较差 absolute black body 绝对黑体 absolute ceiling 绝对云幕高 absolute coordinate system 绝对坐标系 absolute drought 绝对乾旱 absolute error 绝对误差 absolute extremes 绝对极端值 absolute frequency 绝对频率 absolute gradient current 绝对梯度流 absolute humidity 绝对溼度 absolute index of refraction 绝对折射率 absolute instability 绝对不稳度 absolute instrument 绝对仪器 absolute isohypse 绝对等高线 absolute linear momentum 绝对线性动量 absolute momentum 绝对动量 absolute monthly maximum temperature 绝对月最高温 absolute monthly minimum temperature 绝对月最低温 absolute motion 绝对运动 absolute parallax 绝对视差 absolute parcel stability 绝对气块稳度 absolute potential vorticity 绝对位涡 absolute pyrheliometer 绝对日射强度计 absolute reference frame 绝对坐标系 absolute refractive index 绝对折射率 absolute scale 绝对标度 absolute scale of temperature 温度绝对标度 absolute stability 绝对稳度 absolute standard barometer 绝对标準气压计 absolute temperature 绝对温度 absolute temperature scale 绝对温标 absolute topography 绝对地形 absolute unit 绝对单位 absolute vacuum 绝对真空 absolute value
    [Show full text]