什么是急流？
What is a jet stream?
急流是高空西风带中狭窄、强而快的西风气流带，风速可超过每小时300公里。它位于温度梯度大的锋区上方，对地面气旋路径和航空飞行都有重要影响。
A jet stream is a narrow, fast ribbon of westerly wind high in the atmosphere, with speeds exceeding 300 km/h. It lies above sharp temperature gradients at frontal zones and strongly influences surface storm tracks and aviation routes.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#急流 #高空风 #西风带
极锋理论如何解释中纬度气旋的生命周期？
How does polar front theory explain the life cycle of mid-latitude cyclones?
极锋理论由比耶克尼斯在1919年提出，把中纬度气旋看作极地冷气团与热带暖气团交界面上发展的波动。气旋沿锋面成长、产生暖锋与冷锋，并在锢囚阶段达到最强后逐渐填塞。这一理论奠定了现代天气图分析与预报的基础。
Bjerknes proposed polar front theory in 1919, viewing mid-latitude cyclones as waves developing along the boundary between polar cold and tropical warm air masses. A cyclone grows along the front, spawning warm and cold fronts, peaks at occlusion, then fills. The theory founded modern weather-map analysis and forecasting.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#极锋理论 #气旋 #锋面
急流为什么出现在大约十公里高的天空？
Why do jet streams occur around 10 km up in the sky?
急流位于不同温度气团交界（如极地冷气团与副热带暖气团）附近，温度梯度大导致强气压梯度，再加上高空摩擦小，于是形成狭窄的高速西风带。
Jet streams sit near boundaries of very different temperatures (polar vs subtropical air); the large temperature gradient drives a strong pressure gradient, and with little friction aloft, a narrow fast westerly wind forms.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
盛裴轩等,《大气物理学》,北京大学出版社,2003
Sheng Peixuan et al., Atmospheric Physics, Peking University Press, 2003
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787301063019（豆瓣书目条目: 大气物理学）
#急流 #温度梯度
什么是“厄尔尼诺—南方涛动”（ENSO）？它怎样影响全球气候？
What is the El Niño–Southern Oscillation (ENSO), and how does it affect global climate?
ENSO是热带中东太平洋海表温度与大气气压的周期性异常：厄尔尼诺时该区海温异常偏暖、信风减弱，拉尼娜时则偏冷、信风增强。“南方涛动”一名由吉尔伯特·沃克（Gilbert Walker）在1920年代提出，该现象会通过大气遥相关改变全球的降雨与干旱格局。
ENSO is the periodic fluctuation of sea-surface temperature and atmospheric pressure in the tropical central-eastern Pacific: El Niño brings unusually warm waters and weakened trade winds, while La Niña brings the opposite. The term 'Southern Oscillation' was coined by Gilbert Walker in the 1920s, and the phenomenon shifts global rainfall and drought patterns through atmospheric teleconnections.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#厄尔尼诺 #拉尼娜 #南方涛动 #沃克 #遥相关
飓风的能量来自哪里？
Where does a hurricane get its energy?
温暖海面蒸发的水汽在高空凝结放热，像发动机燃料不断供能，海温低于26℃便难以维持。
Latent heat from evaporating warm seawater powers the storm; below 26°C it weakens.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#飓风 #能量
为什么最常见的日晕半径约为22°,而且内侧偏红、外侧偏蓝紫?
Why does the commonest solar halo have a radius of about 22°, and why is its inner edge reddish while its outer rim is bluish?
22°晕是阳光穿过大气中随机取向的六方柱状冰晶发生折射形成的。光线经过夹角为60°的两个晶面时,能量集中在最小偏向角附近——红光约21.8°,蓝紫光约22.4°,于是围绕太阳出现半径约22°的明亮光环。短波长的光偏向角更大而被排到环的外侧,红光留在内侧,晕因此呈现内红外蓝的色彩顺序。
The 22° halo forms when sunlight refracts through randomly oriented hexagonal columnar ice crystals in the air. Rays crossing two crystal faces that meet at 60° concentrate near the minimum-deviation angle, about 21.8° for red light and 22.4° for violet, so a bright ring of roughly 22° radius encircles the Sun. Shorter wavelengths deviate more strongly and are displaced outward, leaving red on the inside and giving the halo its characteristic colour order.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 来源待核验 · Source pending review
来源 · Source
出处备注：作者 / 书名 / 版次 / 出版社 / 年份齐备，仅缺独立比对证据；已在可信度报告单列披露，不再重复核验。
R. Greenler,《虹、晕与幻日》(Rainbows, Halos, and Glories),Cambridge University Press,1980年,第5章
Robert Greenler, Rainbows, Halos, and Glories, Cambridge University Press, 1980, Chapter 5
#大气光象 #冰晶晕
闪电放电为什么能在数毫秒内把通道里的空气加热到约3万K,比太阳表面还要热?
How can a lightning discharge heat the air in its channel to about 30,000 K within milliseconds, hotter than the surface of the Sun?
雷暴云内的电荷分离可建立上亿伏的电位差,击穿后先导通道开辟出直径仅几厘米的高导电通路,紧随其后的回击电流峰值通常达20至30千安。如此巨大的电流挤在极小的截面里,靠焦耳热在微秒量级内把稀薄空气加热到约30000 K,通道气压骤增并向外推出冲击波。这道冲击波传到人耳,就是我们听到的雷声。
Charge separation inside a thundercloud builds potential differences of hundreds of megavolts; once breakdown occurs, the leader carves a conductive channel only centimeters wide, and the following return stroke carries peak currents of roughly 20-30 kA. Forcing that current through such a tiny cross section deposits Joule heat fast enough to raise the thin air to about 30,000 K in microseconds, and the sudden pressure rise drives a shock wave outward. That shock is what reaches our ears as thunder.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-10-04
来源 · Source
Rakov V. A. 与 Uman M. A.,《Lightning: Physics and Effects》,剑桥大学出版社,2003年,第4章与第11章
Rakov V. A. & Uman M. A., Lightning: Physics and Effects, Cambridge University Press, 2003, Chs. 4 and 11
独立核验依据 · Independent verification: 核验依据 1 ISBN 9780486150956 (2003)
#闪电物理 #雷电回击
什么是露点温度？
What is the dew point temperature?
露点是在恒定气压下空气冷却到饱和、开始凝结出水汽所对应的温度，反映空气中实际的水汽含量。露点越高说明空气越潮湿，当气温降至露点以下时常出现雾、露或云。
The dew point is the temperature to which air must cool at constant pressure to become saturated and begin condensing moisture, reflecting its actual water vapor content. A higher dew point means more humid air, and when air temperature drops to the dew point, fog, dew, or clouds form.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#露点 #湿度 #饱和
飓风（台风）是如何形成的？
How do hurricanes (typhoons) form?
飓风在温暖（约26℃以上）的洋面上形成，海面水汽上升释放潜热，使中心气压降低并旋转增强，最终发展为具风眼的风暴。它们在东亚称台风，在美洲附近称飓风。
Hurricanes form over warm ocean water above about 26°C, where rising moisture releases latent heat, lowering central pressure and spinning the system up into a storm with an eye. They are called typhoons in East Asia and hurricanes near the Americas.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#飓风 #台风 #暖洋面
什么是“科里奥利效应”？它如何影响风和洋流？
What is the Coriolis effect, and how does it affect winds and ocean currents?
科里奥利效应源于地球自转：在旋转的地球上，运动的物体（如风、洋流）在北半球向右偏、南半球向左偏。它使全球风带和洋流呈旋转状分布，也是热带气旋旋转方向（北半球逆时针、南半球顺时针）的原因。
The Coriolis effect arises from Earth's rotation: moving objects such as winds and currents are deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. It shapes global wind belts and ocean gyres and determines the spin direction of tropical cyclones (counterclockwise north, clockwise south).
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#科里奥利效应 #地球自转 #风向偏转 #洋流 #气旋
季风是什么？为什么亚洲季风显著？
What is a monsoon, and why is Asia's monsoon so strong?
季风是随季节反转的大范围风向变化，主要由海陆热力差异驱动。亚洲拥有世界最大陆地（欧亚大陆）和最大海洋（太平洋），夏季陆地升温快形成低压吸引海洋湿润气流，故季风特别强盛。
A monsoon is a large-scale seasonal reversal of wind direction, mainly driven by land-sea thermal contrasts. Asia sits between the huge Eurasian landmass and the Pacific Ocean; in summer the land heats fast, forming low pressure that draws in moist ocean air, making its monsoon especially strong.
难度 进阶 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#季风 #海陆差异 #亚洲
什么是龙卷风？
What is a tornado?
龙卷风是从雷暴云底伸向地面的高速旋转气柱，风力极强、破坏集中。它常伴随超级单体风暴，在美国中部平原尤为常见。
A tornado is a rapidly spinning column of air extending from a thunderstorm to the ground, with intense concentrated destructive winds. It often forms with supercell storms and is especially common on the central U.S. plains.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#龙卷风 #超级单体 #气旋
飓风的风眼是什么？
What is the eye of a hurricane?
风眼是飓风中心一片相对平静、少云无风的圆形区域，被周围高耸的眼墙所包围。眼墙内风雨最猛，穿过风眼后会遭遇另一侧同样强烈的天气。
The eye is a relatively calm, clear, low-wind circle at a hurricane's center, ringed by the towering eyewall. The eyewall holds the storm's fiercest winds and rain, and the other side brings equally violent weather after the eye passes.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#风眼 #眼墙 #飓风结构
为什么急流弯成大波浪时，天气容易出极端情况？
Why does a wavy jet stream lead to extreme weather?
当急流蜿蜒成深槽和高压脊，冷暖空气被拉得很南北分明，槽前易暴雨、脊下易热浪干旱，若系统停滞就会让某地连着极端天气。
When the jet meanders into deep troughs and ridges, cold and warm air separate sharply; troughs bring storms, ridges bring heat and drought, and if the pattern stalls, extremes persist in one place.
难度 进阶 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#急流波 #阻塞
季风是什么，亚洲季风为何如此强大？
What is a monsoon, and why is the Asian monsoon so powerful?
季风是随季节反转的大尺度风系，根源是海陆间巨大的热力差异造成气压季节性反转。亚洲拥有最高耸的青藏高原与最广袤的陆地，夏季大陆剧烈增温形成强低压，把印度洋湿空气吸向内陆。韦伯斯特在2006年对亚洲季风的机制与变率做了综合论述。
A monsoon is a seasonal reversal of large-scale winds rooted in the huge thermal contrast between land and ocean that flips pressure patterns. Asia combines the towering Tibetan Plateau with the largest landmass, so summer heating creates a strong low that draws moist Indian Ocean air inland. Webster synthesized the Asian monsoon's mechanics and variability in 2006.
难度 进阶 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-11-03
来源 · Source
王斌(Bing Wang)、傅泰夫(Taifu Fu)主编,The Asian Monsoon,Springer,2008
Bing Wang and Taifu Fu (eds.), The Asian Monsoon, Springer, 2008
独立核验依据 · Independent verification: 核验依据 1 OPENLIBRARY 标识 /works/OL5559659W：The Asian Monsoon（首版 20
#季风 #亚洲季风 #海陆热力差异
气旋和反气旋有什么不同？
What is the difference between a cyclone and an anticyclone?
气旋是中心气压低、空气向内辐合并上升的天气系统，北半球逆时针旋转，常带来阴雨。反气旋中心气压高、空气向外辐散下沉，北半球顺时针旋转，多晴朗干燥天气。
A cyclone is a low-pressure system where air converges inward and rises, rotating counterclockwise in the Northern Hemisphere and often bringing clouds and rain. An anticyclone is a high-pressure system with diverging sinking air, rotating clockwise northward and bringing clear, dry weather.
难度 进阶 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#气旋 #反气旋 #气压
龙卷风是如何形成的，中纬度为何是其高发区？
How does a tornado form, and why are mid-latitudes its hotspot?
龙卷风源于强雷暴中的中气旋，当上升气流与风切变使暖湿与干冷空气剧烈旋转，便可能下伸成漏斗。中纬度常是冷干极地气团与暖湿热带气团交锋之地，提供了最易产生超级单体的环境条件。马科夫斯基与理查森在2009年综述了龙卷形成的物理机制。
A tornado develops from a mesocyclone within a strong thunderstorm, where updrafts and wind shear make warm-moist and dry-cold air rotate violently and stretch into a funnel. Mid-latitudes are where cold polar and warm tropical air masses collide, yielding the classic environment for supercells. Markowski and Richardson reviewed tornado-genesis physics in 2009.
难度 进阶 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#龙卷风 #中气旋 #超级单体
太阳或月亮周围的22°光环是怎样形成的?为什么它常被当作降雨的前兆?
What produces the ring of light at 22 degrees around the Sun or Moon, and why is it often taken as a sign of approaching rain?
高云中的六棱柱状冰晶在随机翻滚取向下,阳光经晶体相邻两个侧面发生折射,透射光集中在最小偏向角约22°处最亮,形成内缘锐利的光环。由于折射色散,晕的内侧偏红、外侧渐变为蓝紫色。卷云往往是一整套锋面雨带最先抵达的高云,因此民间日晕主雨的经验说法具备一定的天气学依据。
Hexagonal prism ice crystals tumbling randomly in high cloud refract sunlight through two adjacent side faces, and the transmitted light peaks near the minimum deviation angle of about 22 degrees, drawing a bright ring with a sharp inner edge. Because refraction disperses wavelengths, the halo's inner rim appears reddish and shades outward through blue and violet. Cirrostratus sheets usually arrive ahead of an approaching frontal system, which gives folk sayings linking halos to imminent rain a real meteorological footing.
难度 进阶 · 适合 大众
CC BY 4.0 · 来源待核验 · Source pending review
来源 · Source
出处备注：著录仅给书名，无版次与年份；同一书名常对应多个版次，不臆测具体版本。
Les Cowley大气光学网站(atoptics.co.uk);世界气象组织《国际云图集》
Les Cowley's Atmospheric Optics site (atoptics.co.uk); WMO International Cloud Atlas
#六棱柱冰晶折射 #22度晕
闪电的梯级先导是如何一步步打通云地之间的放电通道的?
How does a stepped lightning leader open a discharge channel between cloud and ground step by step?
对流云中霰粒与冰晶碰撞起电,可在云底与地面之间积累出每米数百千伏的强电场。当局部场强逼近空气击穿阈值,先导顶端发射的流光汇聚成直径厘米级、温度上万开尔文的高温通道,以约50米的步长间歇式向下推进。先导一旦接地便触发回击,瞬时电流平均可达30千安左右,通道骤然增亮并激起冲击波,这就是我们听到的雷声。
Collisional charging between graupel and ice crystals inside convective clouds accumulates electric fields reaching hundreds of kilovolts per meter between cloud base and ground. Once the local field nears air breakdown, streamers launched at the leader tip merge into a hot channel centimeters wide at tens of thousands of kelvin, probing downward in intermittent steps of roughly 50 meters. When the leader touches ground it triggers the return stroke, carrying instantaneous currents averaging about 30 kiloamperes; the channel flares brilliantly and drives the shock wave we hear as thunder.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-10-04
来源 · Source
Rakov 与 Uman,Lightning: Physics and Effects,Cambridge University Press,2003
Rakov and Uman, Lightning: Physics and Effects, Cambridge University Press, 2003
独立核验依据 · Independent verification: 核验依据 1 ISBN 9780486150956 (2003)
#闪电物理 #梯级先导
风是怎样形成的？
How does wind form?
风是空气因温度差异造成的气压差而发生的水平流动。当某地空气受热上升、气压降低，周围高压空气就会流过来填补，于是形成了风。
Wind is the horizontal movement of air caused by pressure differences that arise from temperature variations. When air heats and rises, lowering pressure in one place, surrounding higher-pressure air flows in to fill the gap, creating wind.
难度 入门 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#风 #气压 #空气流动
什么是大气压？
What is atmospheric pressure?
大气压是地球大气因重力作用而对地表单位面积施加的压力，海平面平均约为1013百帕。气压的高低变化与天气系统密切相关，低压常带来阴雨，高压多对应晴朗。
Atmospheric pressure is the force exerted by the weight of the air on a unit area of the surface, averaging about 1013 hPa at sea level. Pressure variations link closely to weather: low pressure often brings clouds and rain, while high pressure usually means fair weather.
难度 入门 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#大气压 #百帕 #天气系统
雷阵雨（雷雨）是怎么形成的？
How does a thunderstorm form?
当地面被太阳晒得又热又湿，暖湿空气就会像气球一样往上飘，在高空遇冷变成小水滴和冰晶，聚成乌云。云里的水滴越积越多、相互碰撞，最后变成雨落下来，还会伴随闪电和打雷。
When the ground gets hot and humid, warm moist air rises like a balloon and cools high up, turning into tiny water drops and ice crystals that build a dark cloud. The drops grow and bump together until they fall as rain, often with lightning and thunder.
难度 入门 · 适合 幼儿(3-6)
CC BY 4.0 · 已核验 · Verified 2026-08-23
来源 · Source
Tarbuck & Lutgens,《Earth Science》第14版,Pearson,2015
E. J. Tarbuck and F. K. Lutgens, Earth Science, 14th ed., Pearson, 2015
#雷阵雨 #暖湿空气 #上升 #乌云 #闪电
雾和云有什么相同与不同？
What is similar and different between fog and clouds?
雾和云本质上都是悬浮在近地面或高空的小水滴或冰晶集合。区别在于雾贴近地表、使能见度明显下降，而云悬浮在较高的空中。
Fog and clouds are essentially both collections of tiny water droplets or ice crystals suspended in the air. The difference is that fog hugs the ground and sharply reduces visibility, while clouds float higher up.
难度 入门 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#雾 #云 #能见度
云主要分哪几类？
What are the main types of clouds?
按形态和高度，云主要分为积云（蓬松团状）、层云（均匀层状）和卷云（高空纤细），以及它们的组合如积雨云。不同云类对应不同的天气征兆。
By shape and height, clouds are mainly cumulus (puffy), stratus (layered), and cirrus (wispy, high), plus combinations like cumulonimbus. Different cloud types signal different weather.
难度 入门 · 适合 幼儿(3-6)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#积云 #层云 #卷云
热带气旋为什么要起名字？
Why are tropical cyclones given names?
起名字便于播报和预警，避免混淆，让大家更容易记住和防范某个风暴。
Names make warnings clear and memorable so people can prepare for a specific storm.
难度 入门 · 适合 小学高段(9-12)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#飓风 #命名
天空中常见的云有哪几种？
What are the common types of clouds in the sky?
按高度和形态，云主要分为卷云、积云和层云三大类，再细分为更多类型。例如蓬松像棉花糖的是积云，高空纤细如丝的是卷云，均匀铺满天空的是层云。
By height and shape, clouds are mainly grouped as cirrus, cumulus, and stratus, with many subtypes. For example, puffy cotton-like clouds are cumulus, wispy high-altitude ones are cirrus, and uniform sheets covering the sky are stratus.
难度 入门 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#云 #卷云 #积云 #层云
龙卷风预警和龙卷风注意报有什么不同？
What is the difference between a tornado watch and a warning?
注意报（watch）表示某地区气象条件有利于龙卷风生成，需保持警惕；预警（warning）则表示龙卷风已被雷达或目击确认，已实际发生，应立即避险。
A watch means conditions in an area favor tornado formation, so stay alert; a warning means a tornado has been confirmed by radar or sight and is actually occurring, so take shelter immediately.
难度 入门 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#注意报 #预警 #避险
冰雹是怎样形成的？
How does hail form?
冰雹在强对流云（积雨云）中形成，云内强烈上升气流把水滴反复带到高空冻结、裹上冰层。当冰粒重到上升气流托不住时便落向地面，体积可大可小。
Hail forms inside strong convective clouds (cumulonimbus), where powerful updrafts carry water droplets high into freezing air, adding layers of ice. When the pellet grows too heavy for the updraft, it falls to the ground, varying greatly in size.
难度 入门 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#冰雹 #积雨云 #对流
天气和气候有什么不同？
What is the difference between weather and climate?
天气是某地短时间的冷热阴晴，可能几小时就变；气候则是该地区几十年的平均天气状况。简单说，天气是你每天穿什么，气候是你衣橱里该准备什么。
Weather is the short-term state of the atmosphere in one place, changing within hours; climate is the average weather of a region over decades. Put simply, weather is what you wear today, climate is what your wardrobe should contain.
难度 入门 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#天气 #气候 #平均
龙卷风和飓风有什么不同？
What is the difference between a tornado and a hurricane?
龙卷风是小尺度、生命周期短（几分钟到一小时）、由强雷暴生成的猛烈旋转气柱，常出现在陆地上。飓风（热带气旋）是大尺度、可持续数日、在温暖海面上形成的旋转风暴系统，直径可达数百公里。
A tornado is a small, short-lived (minutes to an hour) violent spinning column spawned by severe thunderstorms, usually over land. A hurricane (tropical cyclone) is a large, long-lasting (days) rotating storm system that forms over warm ocean waters and can span hundreds of kilometers.
难度 入门 · 适合 小学低段(6-8)
CC BY 4.0 · 已核验 · Verified 2026-08-23
来源 · Source
Tarbuck & Lutgens,《Earth Science》第14版,Pearson,2015
E. J. Tarbuck and F. K. Lutgens, Earth Science, 14th ed., Pearson, 2015
#龙卷风 #飓风 #热带气旋 #雷暴 #尺度
闪电和雷声是怎么来的？
What causes lightning and thunder?
雷暴云内电荷分离，当电位差足够大时空气被击穿放电形成闪电，瞬间加热空气使其急剧膨胀发出轰鸣，这就是雷。因为光比声快，我们总是先见闪电后闻雷声。
Inside a storm cloud, separated charges discharge through the air as lightning when the voltage is high enough, and the flash instantly heats the air so it expands explosively into the rumble we call thunder. Light travels faster than sound, so we see lightning before we hear thunder.
难度 入门 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
周淑贞 束炯,《气象学与气候学》第3版,高等教育出版社,1997
Zhou Shuzhen and Shu Jiong, Meteorology and Climatology, 3rd ed., Higher Education Press, 1997
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787040060164（豆瓣书目条目: 气象学与气候学）
#闪电 #雷 #电荷