How to grow a glacier M Jackson

In the 13th Century,

Genghis Khan embarked on a mission
to take over Eurasia,

swiftly conquering countries and drawing
them into his expanding Mongol Empire.

With his vast armies he became almost
unstoppable.

But, legend has it that there was
one obstacle

that even the impressive Khan couldn’t
overcome:

A towering wall of ice,

grown by locals across a mountain pass

to stop the Khan’s armies from
invading their territory.

No one knows how historically accurate
that particular story is,

but remarkably, it draws on fact:

For centuries, in the Karakoram
and Himalayan mountain ranges,

people have been growing glaciers
and using these homemade bodies of ice

as sources of drinking water and
irrigation for their crops.

But before we get to that fascinating
phenomenon,

it’s important to understand the
difference between

glaciers that grow in the wild,

and those that humans create.

In the wild,

glaciers require three conditions to grow:

Snowfall, cold temperatures, and time.

First, a great deal of snow falls and
accumulates.

Cold temperatures then ensure that the
stacked up snow

persists throughout the winter, spring,
summer, and fall.

Over the following years, decades,
and centuries,

the pressure of the accumulated snow

transforms layers into highly compacted
glacial ice.

Artificially growing a glacier,

however, is completely different.

At the confluence of three great
mountain ranges,

the Himalayas, Karakoram, and Hindu Kush,

some local cultures have believed for
centuries that glaciers are alive.

And what’s more,

that certain glaciers can have different
genders including male and female.

Local Glacier Growers ‘breed’ new glaciers
by grafting together—or marrying—

fragments of ice from male and
female glaciers,

then covering them with charcoal,
wheat husks, cloths, or willow branches

so they can reproduce.

Under their protective coverings,

these glacierets transform into fully
active glaciers

that grow each year with
additional snowfall.

Those then serve as lasting
reserves of water

that farmers can use
to irrigate their crops.

These practices have spread
to other cultures,

where people are creating their own
versions of glaciers

and applying them to solve serious
modern challenges around water supplies.

Take Ladakh, a high-altitude desert region
in northern India.

It sits in the rain shadow of the
Himalayas

and receives on average fewer than ten
centimeters of rain per year.

As local glaciers shrink because
of climate change,

regional water scarcity is increasing.

And so, local people have started growing
their own glaciers

as insurance against this uncertainty.

These glaciers come in two types:
horizontal, and vertical.

Horizontal glaciers are formed when
farmers redirect glacier meltwater

into channels and pipes,

then carefully siphon it off into a series
of basins made from stones and earth.

Villagers minutely control the release of
water into these reservoirs,

waiting for each new layer to freeze

before filling the basin
with another wave.

In early spring,

these frozen pools begin to melt,

supplying villagers with
irrigation for their fields.

Local people make vertical glaciers using
the meltwater

from already-existing glaciers
high above their villages.

The meltwater enters channels
that run downhill,

flowing until it reaches a crop site

where it bursts forth from a pipe pointing
straight into the air.

When winter temperatures dip,

this water freezes as it arcs
out of the pipe,

ultimately forming a 50 meter ice
sculpture called a stupa,

shaped like an upside-down ice cream cone.

This inverted form minimizes the amount
of surface area it exposes to the sun

in the spring and summer.

That ensures that the mini-glacier
melts slowly

and provides a reliable supply of water
to feed the farmers’ crops.

These methods may be ancient,

but they’re becoming more relevant

as climate change takes its
toll on our planet.

In fact, people are now growing their own
glaciers in many regions beyond Ladakh.

Swiss people, utilizing modern glacier
growing technology,

created their first stupa in 2016
in the Swiss Alps.

There are plans for over 100 more in
villages in Pakistan,

Kazakhstan, and Kyrgyzstan.

Perhaps one day we’ll be able to harness
our homegrown glaciers

well enough to build whole walls of ice–

this time not for keeping people out,

but to enable life in some of the planet’s
harshest landscapes.

在 13 世纪,

成吉思汗开始了一项
接管欧亚大陆的任务,

迅速征服了各个国家,
并将它们纳入他不断扩张的蒙古帝国。

凭借他庞大的军队,他几乎
势不可挡。

但是,传说有
一个障碍

,即使是令人印象深刻的可汗也无法
克服

:一堵高耸的冰墙,

由当地人在山口种植,

以阻止可汗的军队
入侵他们的领土。

没有人知道
这个特定的故事在历史上有多准确,

但值得注意的是,它借鉴了一个事实:

几个世纪以来,在喀喇昆仑
山脉和喜马拉雅山脉,

人们一直在种植冰川,
并使用这些自制的冰体

作为饮用水和
灌溉的来源。 他们的庄稼。

但在我们了解这一迷人
现象之前

,了解

在野外生长的冰川

与人类创造的冰川之间的区别很重要。

在野外,

冰川需要三个条件才能生长:

降雪、低温和时间。

首先,大量的雪落
下来并堆积起来。

然后寒冷的温度确保
积雪

在整个冬季、春季、
夏季和秋季持续存在。

在接下来的几年、几十年
和几个世纪里,

积雪的压力

将层层转变为高度压实的
冰川冰。 然而,

人工培育冰川

则完全不同。

喜马拉雅山脉、喀喇昆仑山脉和兴都库什山脉三大山脉的交汇处,

一些当地文化
几个世纪以来一直相信冰川是有生命的。

更重要的是

,某些冰川可以有不同的
性别,包括男性和女性。

当地的冰川种植者
通过将雄性和雌性冰川的冰块嫁接或嫁接来“培育”新冰川

然后用木炭、
麦壳、布或柳枝覆盖它们,

以便它们能够繁殖。

在它们的保护层下,

这些冰川转变为完全
活跃的冰川

,每年都会随着
额外的降雪而增长。

然后这些作为持久
的水储备

,农民可以
用来灌溉庄稼。

这些做法已经传播
到其他文化,

人们正在创造自己
的冰川版本

,并将其应用于
解决供水方面的严重现代挑战。

以印度北部的高海拔沙漠地区拉达克为例

它位于喜马拉雅山的雨影中

,每年平均降雨量不到十
厘米。

随着当地冰川
因气候变化而缩小,

区域水资源短缺正在加剧。

因此,当地人已经开始种植
自己的冰川,

以应对这种不确定性。

这些冰川有两种类型:
水平的和垂直的。


农民将冰川融水重新引导

到渠道和管道中,

然后小心地将其吸入一系列
由石头和泥土制成的盆地时,就会形成水平冰川。

村民们仔细控制
向这些水库放水,

等待每一层新水层结冰,

然后
再用另一波水填满盆地。

在早春,

这些结冰的水池开始融化,

为村民
们的田地提供灌溉。

当地人

利用村庄上方已有冰川的融水制造垂直冰川。

融水进入
下坡的通道,

一直流到农田

,然后从一根直通空气的管道中喷涌
而出。

当冬季气温下降时,

这些水会结冰,因为它会
从管道中流出,

最终形成一个 50 米长的冰雕,
称为佛塔,

形状像一个倒置的冰淇淋蛋筒。

这种倒置的形式最大限度地减少了
它在春季和夏季暴露在阳光下的表面积

这确保了迷你冰川
缓慢融化,

并为
农民的庄稼提供可靠的水源。

这些方法可能很古老,

随着气候变化
对我们的星球造成影响,它们变得越来越重要。

事实上,人们现在正在
拉达克以外的许多地区种植自己的冰川。

瑞士人利用现代冰川
生长技术,

于 2016 年在瑞士阿尔卑斯山创建了他们的第一座佛塔

巴基斯坦、哈萨克斯坦和吉尔吉斯斯坦的村庄计划再增加 100 多个

也许有一天,我们能够很好地利用
我们本土的冰川

来建造整面冰墙——

这一次不是为了阻止人们进入,

而是为了让地球上一些
最恶劣的景观中的生命得以生存。