Whats below the tip of the iceberg Camille Seaman

Have you ever heard the term,

“tip of the iceberg”?

You know that icebergs
are mostly underwater,

their immense bulk hidden
beneath the water.

But why is that so?

Well, the density of pure ice

is less than that of sea water.

Usually only 1/9
of the volume of an iceberg

is above the water.

The shape of the underwater portion

is difficult to discern

by looking at the above-surface portion.

This has led to the expression,

“tip of the iceberg.”

Here are some thing you might not know

about the icy islands.

The life of an iceberg

begins many thousands of years

before it reaches the ocean.

Unlike sea ice or pack ice,

which form when the ocean freezes,

glaciers are made of fresh water.

For thousands of years,

these glaciers build
layer upon layer of ice,

constantly compressing,

moving,

adding snow,

compressing,

and moving again

as they inch along like a frozen river.

It is the force of gravity

that pulls them towards the sea,

where a glacier may calve
off to become an iceberg

or continue to spread up as an ice shelf

or an ice tongue.

Once an iceberg breaks away

from the glacier or ice shelf,

it will usually live
for three to six years,

floating around, carried by the currents

and tidal movements of the ocean.

As it floats along,

it is battered by waves,

melts,

and smashes into land

and sometimes other icebergs.

Some icebergs are so unstable

that they have more dramatic ends,

heaving up,

collapsing,

and sometimes even exploding.

And as they fall apart,

many icebergs make all sorts
of strange sounds.

When a piece of iceberg melts,

it makes a fizzing sound,

called Bergie Seltzer.

This sound is made when
the water-ice interface

reaches compressed air
bubbles trapped in the ice.

As this happens, each bubble bursts,

making a popping sound.

There are six official size
classifications for icebergs.

The smallest icebergs are called growlers.

They can be up the size of your car

and are very dangerous for ships and boats

because usually they sit
just at the waterline

where they are not easy to spot.

Next are the bergy bits

  • yes, that is their scientific name -

which can be up to the size of your home.

The other four sizes are small,

medium,

large,

and very large.

So just how big is a very large iceberg?

Officially, any iceberg looming larger

than 270 feet high above sea level

and 670 feet long

is considered very large.

That’s 27 stories of looming, blue ice.

And how do icebergs get
that blue color anyways?

When snow on the glacier

is compressed over many hundreds of years,

the weight of the snow

forces the air bubbles out of the ice,

creating pure ice with very
little air trapped inside.

This compression is seen

when the glacier calves,

creating a blue iceberg.

An iceberg that has not experienced

as much compression

and has a large amount
of air and surface edges

reflects light as white.

Although they form in far
northern or southern areas,

icebergs can float thousands of miles.

An iceberg from the Arctic floated

as far south as Bermuda.

Antarctic icebergs are mostly trapped

in the Circumpolar Current,

never giving them a chance to float north.

However, they have been known to interrupt

shipping lanes between Australia,

South America,

and South Africa.

For all their travelling,

many people think

that these slabs of ice
are barren of life,

but these seemingly sterile ice slabs

also harbor their own complex ecosystems

and they shape the ecosystems

that they pass through.

They become mobile, floating ecosystems.

Even in the coldest seas,

icebergs are always melting,

at least a little bit.

This melting has a major impact

on the ocean around an iceberg.

The fresh water from the berg

creates a pool of fresh water

that can extend a nautical
mile away from the iceberg.

This water is colder
than the surrounding sea water,

and the temperature variation
creates thermal currents

in the vicinity of the iceberg.

Life thrives on and around an iceberg.

Young icefish hide in small
ice holes to avoid predators,

while a variety of invertebrates,

like jellyfish and siphonophores,

congregate in the area.

Many of them come to feed on krill,

tiny shrimp-like creatures.

Snow petrels nest on the icebergs

and feed on the sea life nearby.

Whales and seals and penguins
seem to like them too.

And even now that you know all this,

we’re still at the tip of the iceberg.

There are all sorts of things

we don’t know about icebergs.

Perhaps you’ll be
the one to see a little deeper.

你听说过

“冰山一角”这个词吗?

你知道
冰山大部分都在水下,

它们巨大的体积
隐藏在水下。

但为什么会这样呢?

嗯,纯冰的密度

小于海水的密度。

通常只有 1/9
的冰山

体积在水面之上。

水下部分的

形状很难

通过观察水面部分来辨别。

这导致了

“冰山一角”的表达。

这里有一些你可能不知道的

关于冰冷岛屿的事情。

冰山的生命

在它到达海洋之前几千年就开始了。

与海洋结冰时形成的海冰或浮冰不同

冰川是由淡水构成的。

几千年来,

这些冰川
层层积冰,

不断压缩、

移动、

加雪、

压缩,

然后再次移动

,就像一条冰冻的河流一样缓慢移动。

正是重力

将它们拉向大海,

那里的冰川可能会
崩解成冰山,

或者继续向上扩展为冰架

或冰舌。

一旦冰山

脱离冰川或冰架,

它通常会

洋流和潮汐运动的作用下四处漂浮,存活三到六年。

当它漂浮时,

它会受到海浪的冲击,

融化

并撞击陆地

,有时还会撞击其他冰山。

一些冰山非常不稳定

,以至于它们的结局更加戏剧化,会

上升、坍塌

,有时甚至会爆炸。

当它们分崩离析时,

许多冰山会发出
各种奇怪的声音。

当一块冰山融化时,

它会发出嘶嘶声,

称为 Bergie Seltzer。

当水-冰界面

到达
被困在冰中的压缩气泡时,就会发出这种声音。

当这种情况发生时,每个气泡都会破裂,

发出爆裂声。 冰山

有六种官方尺寸
分类。

最小的冰山被称为咆哮者。

它们的大小可能与您的汽车一样大,

并且对船舶非常危险,

因为它们通常
位于

不容易发现的吃水线处。

接下来是 bergy bits

  • 是的,这是他们的学名

  • 可以达到你家的大小。

其他四种尺寸分别为小、

中、

和超大。

那么一个非常大的冰山到底有多大?

正式地,任何

高于海平面 270 英尺

和 670 英尺长的冰山都

被认为是非常大的。

那是 27 层隐约可见的蓝色冰层。

无论如何,冰山
是如何获得蓝色的?

当冰川上的雪

在数百年内被压缩时,

雪的重量

会将气泡从冰中挤出,

形成纯净的冰,
里面几乎没有空气。

这种压缩

在冰川崩塌

形成蓝色冰山时可见。

一座没有经历

过如此大的压缩

并且有
大量空气和表面边缘的冰山

反射出白色的光。

尽管它们形成于遥远的
北部或南部地区,但

冰山可以漂浮数千英里。

北极的冰山漂浮

在最南边的百慕大。

南极冰山大多被困

在绕极流中,

从来没有给它们向北漂浮的机会。

然而,众所周知,它们会中断

澳大利亚、

南美

和南非之间的航道。

在他们所有的旅行中,

许多人

认为这些冰层
是贫瘠的生命,

但这些看似贫瘠的冰层

也拥有自己复杂的生态系统

,它们塑造了

它们所经过的生态系统。

它们变成移动的、漂浮的生态系统。

即使在最寒冷的海域,

冰山也总是在融化,

至少有一点。

这种融化

对冰山周围的海洋产生了重大影响。

来自冰山

的淡水形成了一个淡水池

,可以
从冰山延伸一海里。

这种水
比周围的海水更冷

,温度变化

在冰山附近产生热流。

生命在冰山上和周围茁壮成长。

年轻的冰鱼躲在
小冰洞中以躲避捕食者,

而各种无脊椎动物,

如水母和虹吸管,则

聚集在该地区。

他们中的许多人来以磷虾为食,这种

微小的虾状生物。

雪海燕在冰山

上筑巢,以附近的海洋生物为食。

鲸鱼、海豹和企鹅
似乎也喜欢它们。

即使现在你知道了这一切,

我们仍然处于冰山一角。

关于冰山,有很多我们不知道的事情。

也许你会
是一个看得更深的人。