How to track a tornado - Karen Kosiba

79,100 views ・ 2014-04-21

TED-Ed


請雙擊下方英文字幕播放視頻。

譯者: Wei Chang 審譯者: Max Chern
00:06
So, I think all good tornado talks need to start
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我想每個關龍捲風的優秀演講
都是用精彩的龍捲風相片作為開頭
00:09
with an awesome tornado shot.
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00:11
And this is not that awesome tornado shot.
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但這張並不是那種精彩的龍捲風相片
00:13
That was the first tornado I ever saw, it was really cool, really scary,
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這是我第一次看見的龍捲風
很酷、很可怕
00:16
and I'm showing it to you guys
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我把這張相片展示給你們看
因為這是我起初進入這領域的理由
00:18
because that's why I got into the field in the first place.
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所以即使這張照片沒拍好
00:21
So even though it's a bad photograph,
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00:22
it was really cool to be out there the first time.
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能第一次親眼見到龍捲風還是很酷
不過現在我在拍的是真正的龍捲風影片
00:25
But now I'm taking real tornado footage.
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00:27
Fast forward a few years.
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向前快轉幾年
00:28
This is a few years ago, during a field project called VORTEX2,
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幾年前,我參與一個
名為 VORTEX2 的實地勘查計畫
00:32
where myself and a bunch of other scientists were out there,
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我和一群科學家一起
帶著各種儀器圍著龍捲風
00:35
surrounding tornadoes with different types of instrumentation
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00:37
and trying to figure out how tornadoes form.
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試著找出龍捲風的成因
00:40
It's a big question we're trying to answer.
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那是我們試圖回答的大哉問
00:42
It sounds like a very basic one,
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聽起來很基本
00:43
but it's something we're still trying to figure out.
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但我們仍在努力找出答案
我們也想了解
00:46
We're also still trying to figure out what the winds are like near the surface.
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靠近地表的地方,風是怎麼吹的
00:49
We know what the winds are like above building level,
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我們知道建築高度以上的風如何運作
但我們真的不知道地表處的情形
00:52
but we really don't know what they're like at the surface
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以及這兩者之間的關聯
00:55
and how that relates to what we're seeing above building level.
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大部分的龍捲風成形於超大胞雷暴
00:58
Most tornadoes form from what we call supercell thunderstorms.
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01:01
Supercell thunderstorms are what you commonly think of
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超大胞雷暴一般會被想成
帶來龍捲風的風暴
01:04
as tornado-raising storms.
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01:05
They're big, rotating thunderstorms
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那是大型、會旋轉的雷暴
01:07
that happen a lot of times in the midsection of the United States.
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常常發生在美國中部
01:10
But the problem is that even though they're rotating up above,
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但問題是,即使它們上層正在旋轉
01:14
it doesn't mean they're rotating at the surface.
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不代表靠近地表的地方也有在轉
當我們研究這些風暴
01:16
And when we look at these storms
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這些照片、這些我們手中的資料
01:18
and at these pictures and at the data we have,
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01:20
they all kind of look the same.
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它們看起來好像都一樣
當我們試著發佈龍捲風預報或警告
01:22
And it's really problematic
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01:23
if we're trying to make tornado forecasts or warnings,
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就會產生許多問題
01:25
because we only want to warn or forecast about the storms
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因為我們只想要預警或預測
01:28
that are going to actually make a tornado.
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那些真的會形成龍捲風的風暴
01:30
One of the big, critical distinguishing features, we think, between these storms,
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我們認為,這些風暴之間 最大、最關鍵的區別
和後側緣下沉氣流有關
01:35
is something about the rear-flank downdraft.
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01:37
So these big rotating thunderstorms have this downdraft
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這種下沉氣流
環繞在這些大型旋轉的雷暴雨的後側邊緣
01:40
that wraps around the rear edge of it,
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01:42
hence the "rear-flank" downdraft.
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因此被稱為「後側緣」下沉氣流
01:44
But we think how warm that is, how buoyant that air is,
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我們也認為其溫度、空氣浮力
01:47
and then also how strong the updraft it's wrapping into,
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以及上升氣流將空氣吸入的力度
01:51
makes a big difference on whether or not it's going to make a tornado.
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都與龍捲風是否能形成息息相關
01:54
There's a lot more that goes into it --
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還有更多需要考慮的事情
01:56
I'll tell you about that in a second.
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我馬上就會告訴你們
一旦龍捲風確實再次成形
01:58
Once you actually get a tornado, again, the problem that we have
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我們要思考的問題就變成
02:01
is getting measurements near the surface.
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要如何測量靠近地表的數據
02:03
It's really hard to get measurements near the surface --
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要能得到靠近地表的數據真的很難--
人大多不會願意開車闖進龍捲風中
02:06
most people don't want to drive into tornadoes.
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02:08
There are a few exceptions; you might have seen them on TV shows.
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當然有些例外, 你可能在電視節目中看過
02:11
But most people don't want to do that.
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但大部分的人都不會想這麼做的
02:13
Even getting instrumentation in the path of the tornado is pretty tricky, too.
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要把儀器放到龍捲風 行經路徑上也不容易
02:17
Because, again, you don't want to be that close to a tornado
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因為,同樣地,你不會想離龍捲風那麼近
有時候龍捲風附近的風也很強勁
02:20
because sometimes the winds around the tornado are strong as well.
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所以能得到確切位置的資訊 對我們來說很重要
02:23
So getting information, that critical location,
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02:25
is key for us because, again, we don't know
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因為我們不知道
02:27
if the winds that we're seeing above ground level,
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我們在地表高度以上、建築高度以上
02:30
way above building level,
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02:31
actually map to the surface,
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所看見的是否與地面相符
02:32
if they're stronger, weaker, or about the same
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不知道地面的風是否比建築高度以上
02:35
as what we're seeing above buildings.
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強、弱,還是一樣
02:37
The way we get at answering a lot of these questions --
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我們尋求這麼多問題解答的方式--
02:40
and I'm an observationalist; I love to get out in the field,
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我是名觀察學者,我喜歡實地勘查
收集龍捲風有關的資料
02:43
and collect data on tornadoes --
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--我們彙整了許多觀察結果
02:44
we compile a lot of observations.
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我和一個團隊合作, 他們會操作機動雷達
02:46
I work with this group who operates mobile radars,
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02:48
and they're exactly what they say -- basically, a radar
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而他們就像他們自己所描述的--
基本上就是一台載著雷達的藍色卡車
02:51
on the back of a big blue truck,
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02:52
and we drive up really close to tornadoes to map out the winds.
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我們會開到離龍捲風很近的地方, 記錄風
02:55
We map out the precipitation.
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記錄降雨
02:57
We map out all these different things that are going on
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記錄發生的一切事物
03:00
in order to better understand the processes in these storms.
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以能更清楚地理解這些風暴的過程
底下這張照片
03:03
And that bottom there, that's what a tornado looks like
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當你很靠近龍捲風並用雷達觀測它時
03:05
when you're looking at it with a mobile radar, and really close.
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它看起來就是這樣子
03:09
Also, what we do is a lot of modeling,
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我們常做的事情還有建構模組
03:11
so we do a lot of computer models and simulations,
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所以我們在電腦上 建構很多模組、進行模擬
03:14
because the atmosphere is governed by the laws of physics.
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因為大氣層受到物理法則制約
所以我們可以依據物理法則建模
03:17
So we can model the laws of physics
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03:18
and see where the tornado might go,
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看看龍捲風可能會怎麼移動
03:20
where the storm might go,
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風暴怎麼移動
03:22
how strong the winds are near the surface
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接近地表的風會有多強
03:24
and not actually have to go out in the field.
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而無需真正進入現場
03:26
But of course, we want to have both observations and modeling
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但是,我們當然想要觀察和建模並進
03:29
to move forward with the science.
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讓兩者一起推動科學前進
這和我稍早之前給你們看的影片一樣
03:31
So, I showed you that video earlier that went real quick, too.
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移動得很快速
03:34
This is what it looks like, looking at it with a radar.
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這是那個影片在雷達上呈現的樣貌
03:37
So you saw it visually,
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所以你用雙眼看見它了
03:38
but this is what I get really excited about when I see now in the field,
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但如今會讓我真的興奮起來的
是在現場看見像這樣的圖
03:42
stuff that looks like this.
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看見這樣的圖會讓我們興奮的原因是
03:43
The really exciting thing about looking at stuff like this
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我們在風暴尚未形成龍捲風前 捕獲到它了
03:46
is that we caught this storm from when it didn't make a tornado
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03:49
to when it made a tornado and intensified
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記錄到龍捲風形成、加劇
03:51
and when it dissipated.
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以及它消散的時刻
03:52
This is the one of the rare data sets that we have out there
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這是我們在實地勘查過程中 罕見能得的資料
03:55
that were able to study the entire life cycle of a tornado.
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我們可以藉此研究龍捲風完整的生成週期
03:58
I talked about how we think that rear-flank downdraft is important
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我提過我們認為後側緣下沉氣流很重要
04:02
because it tilts, there's a lot of spin in the atmosphere,
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因為它是傾斜的
大氣層中有許多旋轉氣流
04:05
but the problem with all this spin in the atmosphere
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但問題是所有這些旋轉的氣流
04:07
is it needs to be oriented vertically,
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方向必須要是垂直的
04:09
because that's what tornadoes are doing,
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因為那是龍捲風運作的方式
04:11
and it needs to orientated vertically near the ground.
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在接近地表的地方,方向要是垂直的
所以我們認為 這種後側緣下沉氣流如同脈搏
04:14
So we think this rear-flank downdraft just pulses.
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04:17
And these pulses in this rear-flank downdraft, we think,
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這些後側緣下沉氣流中的脈搏
04:19
are very important for converging that rotation,
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對聚集旋轉氣流而言非常重要
04:22
but also getting that rotation into the right place.
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也能讓這些旋轉氣流進到該去的位置
我們認知到另一件事
04:25
Other things we've learned
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04:26
is that we have gotten a bunch of fortuitous measurements
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在龍捲風行經路徑上 和非常接近地面的地方
04:29
in the path of the tornadoes and very near the surface.
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我們取得許多偶然的測量值
04:31
And we found out
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我們發現,在地面附近的風
04:33
that the winds near the surface are actually pretty comparable
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其實和我們在離地面三、四十公尺高
04:36
to what we're seeing 30, 40 meters above ground level.
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所觀察到的差不多
04:38
So there's not a big reduction in what we're seeing above the surface
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我們在地面所見到房屋高度所見
測量值並沒有大幅降低
04:42
to what we're seeing at house level.
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04:43
And that was a pretty surprising finding for us,
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這結果對我們來說滿令人訝異的
因為我們原先滿肯定地認為
04:46
because we kind of assumed that the winds decrease
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風速會在近地面處大幅減少
04:49
pretty substantially near the surface.
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我想很快地用這張圖結束這次演講
04:51
I'm going to end with this real quick.
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04:52
And this is not my last tornado I ever saw,
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這不是我見過的最後一個龍捲風
04:55
but I really like this image,
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但我很喜歡這張圖
04:56
because this was taken with one of those mobile radars I was talking about.
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因為這是用我提到的 其中一台機動雷達拍攝的
這是龍捲風,不是颶風
05:00
This is a tornado, not a hurricane,
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當你真的很靠近它時,它長得像這樣
05:02
and this is what it looks like when you're really close to it.
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我覺得這很神奇
05:05
And I find this amazing,
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我們真的可以運用科技 如此接近這樣的風暴
05:06
that we can actually take technology this close to these types of storms
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05:09
and see these inner workings.
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並且觀察到內部的情形
05:11
And for those of you who look at tornado images often,
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如果你們常看龍捲風的圖片
05:14
you can see there's a lot going on -- there's rain spiraling,
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你們會看出這裡面顯示出很多事情
雨水在螺旋上升
05:17
and you can actually see the debris cloud associated with this tornado.
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也能看見因這場龍捲風出現的碎片雲
我十分期待未來與未來科技
05:20
I look forward to the future and future technologies
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05:22
and being able to learn a lot more about these storms,
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也很期待可以更加了解這些風暴
05:25
as the world advances,
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讓世界更進步
05:26
as you guys contribute to the science
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因為你們對科學有所貢獻
05:28
and we're able to really learn more about how tornadoes form.
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我們能更加了解龍捲風形成的原因
05:31
Thank you.
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謝謝各位!
05:32
(Applause)
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(掌聲)
翻譯:Wei Chang
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