How to track a tornado - Karen Kosiba

如何追踪龙卷风—— Karen Kosiba

79,100 views ・ 2014-04-21

TED-Ed


请双击下面的英文字幕来播放视频。

翻译人员: Cissy Yun 校对人员: Jenny Yang
00:06
So, I think all good tornado talks need to start
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我认为所有关于龙卷风的精彩演讲
都得从一张令人叹服的龙卷风照片开始
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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好吧,那不是一张很棒的龙卷风照片
00:13
That was the first tornado I ever saw, it was really cool, really scary,
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其实,这是我见到的第一个龙卷风
它十分炫酷,但也十分恐怖
00:16
and I'm showing it to you guys
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我之所以想把它展示给你们
是因为它让我第一次走近龙卷风
00:18
because that's why I got into the field in the first place.
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所以,这虽然是一张很烂的照片
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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置身于龙卷风旁还是十分的酷的
如今,我已经在拍摄一些专业的龙卷风视频了
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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快进到几年前
00:28
This is a few years ago, during a field project called VORTEX2,
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当年
在一个实地项目叫做VORTEX2(漩涡2)中
00:32
where myself and a bunch of other scientists were out there,
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我与一 群科学家正处在龙卷风附近
用不同的仪器
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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尝试找出龙卷风形成的原理
我们想找到 一个问题的答案
00:40
It's a big question we're trying to answer.
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这听起来是一个十分基础的问题
00:42
It sounds like a very basic one,
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00:43
but it's something we're still trying to figure out.
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然而,如今我们依旧在寻求其答案
另一个我们想知道的问题是
00:46
We're also still trying to figure out what the winds are like near the surface.
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靠近龙卷风表层的风是怎样吹的
00:49
We know what the winds are like above building level,
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我们已经知道的是楼层高度以上的风是如何运作的
但依旧困扰我们的是龙卷风表层的风向运作
00:52
but we really don't know what they're like at the surface
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以及它是如何与楼层高度之上的龙卷风 联系起来的
00:55
and how that relates to what we're seeing above building level.
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大多数龙卷分都是由“超级单体雷暴”组成的
00:58
Most tornadoes form from what we call supercell thunderstorms.
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这种“超级单体雷暴”
01:01
Supercell thunderstorms are what you commonly think of
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就是你们所熟知的 引起龙卷风的风暴
01:04
as tornado-raising storms.
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01:05
They're big, rotating thunderstorms
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它们是一种十分巨大的,旋转型风暴
01:07
that happen a lot of times in the midsection of the United States.
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多发生于美国中部地区
01:10
But the problem is that even though they're rotating up above,
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但问题是
即使这种风暴的上部一直在旋转
01:14
it doesn't mean they're rotating at the surface.
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并不代表它的表层风向也在旋转
01:16
And when we look at these storms
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当我们观察这种风暴
观赏这些图片
01:18
and at these pictures and at the data we have,
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并且研究这些数据时
01:20
they all kind of look the same.
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它们是十分相像的
这种龙卷风存在很多不确定因素
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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当我们想要发出龙卷风预警
01:25
because we only want to warn or forecast about the storms
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我们只是想要对这些风暴发出警告
或是发出将会造成
01:28
that are going to actually make a tornado.
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龙卷风的风暴预警
01:30
One of the big, critical distinguishing features, we think, between these storms,
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一个十分重要的
存在于这些风暴之间的区别
有关一种名为后侧下环流的风
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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这些旋转型风暴的
背部被这种倒灌风包裹着
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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所以被称为后侧下环流
01:44
But we think how warm that is, how buoyant that air is,
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但当我们想到它的温度
它的浮力
01:47
and then also how strong the updraft it's wrapping into,
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以及它的上环流风的力量
将这些总结起
也许就会形成
01:51
makes a big difference on whether or not it's going to make a tornado.
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一个龙卷风
01:54
There's a lot more that goes into it --
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当然,还有其他很多的因素
我一会儿告诉你们
01:56
I'll tell you about that in a second.
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当你真的遇见一个龙卷风时
01:58
Once you actually get a tornado, again, the problem that we have
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对于我们问题就是
02:01
is getting measurements near the surface.
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如何去测量表层的一些数据
02:03
It's really hard to get measurements near the surface --
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测量龙卷风表层数据是十分困难的
多数是因为人们不愿意靠近龙卷风
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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当然,也会有一些例外
也许你们在电视上也看到过一些这样的例子
02:11
But most people don't want to do that.
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但大多数人不会这样做
02:13
Even getting instrumentation in the path of the tornado is pretty tricky, too.
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即使是使用仪器研究龙卷风也会十分困难
02:17
Because, again, you don't want to be that close to a tornado
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当然,你不会想离龙卷风太近
因为龙卷风附近的风也是十分强劲的
02:20
because sometimes the winds around the tornado are strong as well.
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所以获取信息的关键的地点 对我们来说十分重要
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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因为,我们不知道
02:27
if the winds that we're seeing above ground level,
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在地平线以上的风和
02:30
way above building level,
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在楼层高度以上的风
02:31
actually map to the surface,
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是否可以表层的风是有所比对
02:32
if they're stronger, weaker, or about the same
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它们也许比其更强烈,也可能相对微弱
它们也可能和楼层高度以上的风 有相似的强度
02:35
as what we're seeing above buildings.
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02:37
The way we get at answering a lot of these questions --
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我们拥有寻找这些问题的答案的方法
我是一个观察师,所以我喜欢做实地考察
02:40
and I'm an observationalist; I love to get out in the field,
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我也喜欢收集有关龙卷风的数据
02:43
and collect data on tornadoes --
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我们编制了许多观测实例
02:44
we compile a lot of observations.
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我与一组操控"车载雷达"的科学家一起工作
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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正如其名
“车载雷达”基本上就是 安装在一辆蓝色卡车上的雷达
02:51
on the back of a big blue truck,
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我们开着它靠近龙卷风
02:52
and we drive up really close to tornadoes to map out the winds.
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勘察龙卷风以及规划我们的预测
02:55
We map out the precipitation.
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02:57
We map out all these different things that are going on
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我们将所有的的细节都记录下来
为的是更了解这些风暴的形成步骤
03:00
in order to better understand the processes in these storms.
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03:03
And that bottom there, that's what a tornado looks like
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看到左下方的这个图片
这就是龙卷风
03:05
when you're looking at it with a mobile radar, and really close.
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在“车载雷达”中显示出的样子
“车载雷达”需靠龙卷风十分近
03:09
Also, what we do is a lot of modeling,
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我们还会建立许多模型
03:11
so we do a lot of computer models and simulations,
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我们会建立许多电脑模型和拟态
03:14
because the atmosphere is governed by the laws of physics.
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因为大气层是由物理定律控制的
所以我们可以建立关于物理定律的模型
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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然后预测龙卷风的走向
03:20
where the storm might go,
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风暴的走向
03:22
how strong the winds are near the surface
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以及表层风的强度
03:24
and not actually have to go out in the field.
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这样,我们不用去到实地 就可以完成这些考察
但是,我们希望建模和考察能够同时进行
03:26
But of course, we want to have both observations and modeling
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这样会更科学
03:29
to move forward with the science.
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这是一段视频 我前面也给你们看过
03:31
So, I showed you that video earlier that went real quick, too.
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03:34
This is what it looks like, looking at it with a radar.
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这就是通过雷达观测龙卷风时 其所呈现的形态
就是你们现在看到的
03:37
So you saw it visually,
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03:38
but this is what I get really excited about when I see now in the field,
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当时我在在实地考察中看到这个时
我感到很兴奋
可以以这种形态观察龙卷风
03:42
stuff that looks like this.
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这是很振奋人心的一件事
03:43
The really exciting thing about looking at stuff like this
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这个风暴
03:46
is that we caught this storm from when it didn't make a tornado
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当我们捕捉到不同时期的龙卷风 有还未成形的
也有逐渐形成的龙卷风
03:49
to when it made a tornado and intensified
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我们看着它渐渐地增强
然后逐渐地消散
03:51
and when it dissipated.
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03:52
This is the one of the rare data sets that we have out there
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所以,这是我们拥有的一个
十分少见的数据
它可以让我们研究龙卷风的整个形成周期
03:55
that were able to study the entire life cycle of a tornado.
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03:58
I talked about how we think that rear-flank downdraft is important
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我会讲到一种后飞倒灌风
它是一种对我们来说十分重要的风
04:02
because it tilts, there's a lot of spin in the atmosphere,
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因为它会倾斜,并在大气层中不断旋转
04:05
but the problem with all this spin in the atmosphere
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但问题是所以在大气层中的旋转
04:07
is it needs to be oriented vertically,
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都需要是以垂直为中心点
04:09
because that's what tornadoes are doing,
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这也是龙卷风所做的事
04:11
and it needs to orientated vertically near the ground.
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它需要靠近地面作垂直旋转
04:14
So we think this rear-flank downdraft just pulses.
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所以说,当我们想到后飞倒灌风时 我们会将它看作震动
我们觉得很重要的
04:17
And these pulses in this rear-flank downdraft, we think,
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这些震动
04:19
are very important for converging that rotation,
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可以收缩这些旋转
04:22
but also getting that rotation into the right place.
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也会指引龙卷风向正确的方向旋转
04:25
Other things we've learned
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我们学到的另一件事是
04:26
is that we have gotten a bunch of fortuitous measurements
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我们得到了很多关于龙卷风附近
龙卷风表层
04:29
in the path of the tornadoes and very near the surface.
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的一些偶然的数据
04:31
And we found out
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我们发现靠近表层的风
04:33
that the winds near the surface are actually pretty comparable
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是比得上
30,40米高度以上的风
04:36
to what we're seeing 30, 40 meters above ground level.
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04:38
So there's not a big reduction in what we're seeing above the surface
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所以,表层的风并不会比
楼房高度的风弱
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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这是一个比较惊奇的发现
因为,我们以前总是认定
04:46
because we kind of assumed that the winds decrease
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接近表层的风力会相对变弱许多
04:49
pretty substantially near the surface.
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我将会用这张图来结束我的演讲
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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这并非是我见过的最后一个龙卷风
但我十分喜欢这个图片
04:55
but I really like this image,
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04:56
because this was taken with one of those mobile radars I was talking about.
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因为它是由我先前提到的“车载雷达” 所记录下来的
这是一个龙卷风,并非飓风
05:00
This is a tornado, not a hurricane,
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这是当你十分靠近它时
05:02
and this is what it looks like when you're really close to it.
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所呈现的样子
我觉得很惊奇的地方是
05:05
And I find this amazing,
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我们可以运用技术
05:06
that we can actually take technology this close to these types of storms
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来接近这种风暴
05:09
and see these inner workings.
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观察它们的内部
如果你经常看龙卷风的图片
05:11
And for those of you who look at tornado images often,
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05:14
you can see there's a lot going on -- there's rain spiraling,
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你可以发现它包含许多内容
雨水急骤下落, 你甚至可以看到碎片云
05:17
and you can actually see the debris cloud associated with this tornado.
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和龙卷风共存
我十分期望看到未来和新的技术
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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我们可以运用它们来更好的研究这些风暴
05:25
as the world advances,
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随着世界的进步
05:26
as you guys contribute to the science
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当你们投身于科学之中
05:28
and we're able to really learn more about how tornadoes form.
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我们将会获取更多关于龙卷风形成的知识
05:31
Thank you.
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谢谢!
05:32
(Applause)
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