thunderstorm| 有名人の最新ニュースを読者にお届けします。

私たちは、人々が好きな有名人について読んで、それについて気分を良くすることができるスペースを作りたかったのです.私たちは、人々が有名人についてポジティブな方法でゴシップできる場所を作りたかった.
私たちは、何年もの間、日本のエンターテインメント ニュースを生き、呼吸してきた情熱的なエンターテインメント ニュース ジャンキーの小さなチームです。

thunderstorm, 2016-08-03, The Ancients : At Australia’s Spiritual Heart 4K, The Ancients, is not just a time lapse video.It is a saga depicting the spiritual communion of the Oldest of land and the Ethereals above in Red Central Australia. It tells the story of the great spiritual landscape experiencing different seasons across the year.The video features Australian icons that have existed from Devonian to Ediacaran ages ranging from 359-635 million years old.

The old and beautiful Uluru comes face to face with lightning,rain and thunderstorms. The Outback night sky gleams with Millions of stars when the 13.2 billion year old Milky way Galaxy takes the center stage and rises behind Uluru and sets behind Kata Tjuta.Lightning storms batter the landscape, thunderstorms pass above Uluru. Mt conor gets dusted by Sandstorm. Sunsets behind KataTjuta, moonlit landscape at at Ellery Creek waterhole, and McDonnell ranges and much more are part of this video.

The music in the video has slow moody and emotional start and gradually breaks into intense
orchestral music with choral female soprano voice.The music is composed by super talented music producer Ramazan Yuksel. It has been licensed through the links below.
themusicase.com/

Behind the scenes: This video is an outcome of 10 months of footage collection which involved wait,patience,despair and occasional dejection followed by,optimism.hopefulness,face offs with strong weather conditions and equipment breakdown during shooting process.

Equipment and software’s used in the project are listed below.

Camera’s Nikon D750
Lenses,
Nikon 28-300mm
Tokina 16-28mm Atx Pro
Sigma 24-70mm
Tokina 17-35mm
Tripod’s Vanguard 263ATS AltaPro

Motion:
Dynamic Perception Stage One Motion Slider
Dynamic Perception Stage R Pan and Tilt Rotary units
PSE Timelapse Slider

Softwares.
Image Editing :Adobe Lightroom
Time lapse rendering and Deflicker :Timelapse Tool
Video compilation and Editing : CyberLink PowerDirector 14
Star tails Sequences created by : STARSTAX

Conatct: caramelkartikeya@gmail.com
facebook : https://www.facebook.com/KsImagery/

To use this video in a commercial player or in broadcasts, please email licensing@storyful.com, Kartikeya Sharma

thunderstormの学習レベル

詳細については、次の URL をご覧ください。……

thunderstormの使い方と意味

• thunderstorm

  【名】

  激しい雷雨｛らいう｝、雷をともなう豪雨｛ごうう｝

  【レベル】7、【発音】[US] θʌ́ndərstɔ̀rm ｜ [UK] θʌ́ndəstɔ̀ːm、【＠】[US]サンダァストァム、[UK]サンダストーム、【変化】《複》thunderstorms、【分節】thun・der・storm

• thunder-storm

• thunderstorm activities

  → thunderstorm activity

• thunderstorm activity

  雷雨活動｛らいう かつどう｝

• thunderstorm advisories

  → thunderstorm advisory

• thunderstorm advisory

  雷注意報｛かみなり ちゅういほう｝

• thunderstorm alert

  雷雨警報｛らいう けいほう｝

• thunderstorm avoidance

  雷雨回避｛らいう かいひ｝

• thunderstorm cell

  雷雨細胞｛らいう さいぼう｝

• thunderstorm clouds

  積乱雲｛せきらんうん｝

• thunderstorm damage

  雷雨被害｛らいう ひがい｝

詳細については、次の URL をご覧ください。……

目次

• 1 英語
  • 1.1 語源
  • 1.2 発音^(?)
  • 1.3 名詞
    • 1.3.1 略語
    • 1.3.2 上位語
    • 1.3.3 下位語

語源[編集]

複合語 thunder +‎ storm

発音^(?)[編集]

• enPR: thŭn’də(r)-stô(r)m’, IPA: /ˈθʌn.də(ɹ)ˌstɔː(ɹ)m/, IPA: /ˈθʌn.ə(ɹ)ˌstɔː(ɹ)m/
• 押韻: -ɔː(r)m
• 音声(加) :
• 分綴: thun‧der‧storm

名詞[編集]

thunderstorm (複数 thunderstorms)

1. 激（はげ）しい雷雨。

略語[編集]

• t-storm

上位語[編集]

• storm

下位語[編集]

• dirty thunderstorm

詳細については、次の URL をご覧ください。……

thunderstorm

詳細については、次の URL をご覧ください。……

Life cycle

Warm air has a lower density than cool air, so warmer air rises upwards and cooler air will settle at the bottom^[8] (this effect can be seen with a hot air balloon).^[9] Clouds form as relatively warmer air, carrying moisture, rises within cooler air. The moist air rises, and, as it does so, it cools and some of the water vapor in that rising air condenses.^[10] When the moisture condenses, it releases energy known as latent heat of condensation, which allows the rising packet of air to cool less than the cooler surrounding air^[11] continuing the cloud’s ascension. If enough instability is present in the atmosphere, this process will continue long enough for cumulonimbus clouds to form and produce lightning and thunder. Meteorological indices such as convective available potential energy (CAPE) and the lifted index can be used to assist in determining potential upward vertical development of clouds.^[12] Generally, thunderstorms require three conditions to form:

1. Moisture
2. An unstable airmass
3. A lifting force (heat)

All thunderstorms, regardless of type, go through three stages: the developing stage, the mature stage, and the dissipation stage.^[13][14] The average thunderstorm has a 24 km (15 mi) diameter. Depending on the conditions present in the atmosphere, each of these three stages take an average of 30 minutes.^[15]

Developing stage

The first stage of a thunderstorm is the cumulus stage or developing stage. During this stage, masses of moisture are lifted upwards into the atmosphere. The trigger for this lift can be solar illumination, where the heating of the ground produces thermals, or where two winds converge forcing air upwards, or where winds blow over terrain of increasing elevation. The moisture carried upward cools into liquid drops of water due to lower temperatures at high altitude, which appear as cumulus clouds. As the water vapor condenses into liquid, latent heat is released, which warms the air, causing it to become less dense than the surrounding, drier air. The air tends to rise in an updraft through the process of convection (hence the term convective precipitation). This process creates a low-pressure zone within and beneath the forming thunderstorm. In a typical thunderstorm, approximately 500 million kilograms of water vapor are lifted into the Earth’s atmosphere.^[16]

Mature stage

In the mature stage of a thunderstorm, the warmed air continues to rise until it reaches an area of warmer air and can rise no farther. Often this ‘cap’ is the tropopause. The air is instead forced to spread out, giving the storm a characteristic anvil shape. The resulting cloud is called cumulonimbus incus. The water droplets coalesce into larger and heavier droplets and freeze to become ice particles. As these fall, they melt to become rain. If the updraft is strong enough, the droplets are held aloft long enough to become so large that they do not melt completely but fall as hail. While updrafts are still present, the falling rain drags the surrounding air with it, creating downdrafts as well. The simultaneous presence of both an updraft and a downdraft marks the mature stage of the storm and produces cumulonimbus clouds. During this stage, considerable internal turbulence can occur, which manifests as strong winds, severe lightning, and even tornadoes.^[17]

Typically, if there is little wind shear, the storm will rapidly enter the dissipating stage and ‘rain itself out’,^[14] but, if there is sufficient change in wind speed or direction, the downdraft will be separated from the updraft, and the storm may become a supercell, where the mature stage can sustain itself for several hours.^[18]

Dissipating stage

In the dissipation stage, the thunderstorm is dominated by the downdraft. If atmospheric conditions do not support super cellular development, this stage occurs rather quickly, approximately 20–30 minutes into the life of the thunderstorm. The downdraft will push down out of the thunderstorm, hit the ground and spread out. This phenomenon is known as a downburst. The cool air carried to the ground by the downdraft cuts off the inflow of the thunderstorm, the updraft disappears and the thunderstorm will dissipate. Thunderstorms in an atmosphere with virtually no vertical wind shear weaken as soon as they send out an outflow boundary in all directions, which then quickly cuts off its inflow of relatively warm, moist air, and kills the thunderstorm’s further growth.^[19] The downdraft hitting the ground creates an outflow boundary. This can cause downbursts, a potential hazardous condition for aircraft to fly through, as a substantial change in wind speed and direction occurs, resulting in a decrease of airspeed and the subsequent reduction in lift for the aircraft. The stronger the outflow boundary is, the stronger the resultant vertical wind shear becomes.^[20]

詳細については、次の URL をご覧ください。……

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