Author: Simon Winchester
_Simon Winchester_
Reading time: 18 minutes
Synopsis
The Breath of the Gods (2025) looks at how wind changes the world and our daily lives. It talks about travel and exploration, but also about bad events like hurricanes, big fires, and storms. It also checks how global wind patterns are changing and getting stronger because of climate change. And it looks at wind as something that can cause damage, but also as a way to save our planet using clean energy.
What’s in it for me? Understand how wind shapes your life, from gentle breezes to extreme weather and future energy.
Stand outside on what feels like a still day, and you might forget you live at the bottom of an ocean of air. A dandelion breaks in a child’s hand. Smoke moves from a chimney. A plastic bag flies along the street. In all these small movements, you can see invisible wind working quietly.
The air around you is always moving. It connects farms to cities, and mountains to oceans. It links yesterday’s weather to tomorrow’s news. This moving air can cool your skin. It can carry the smell of rain. It can gently move leaves on a tree. But it can also remove soil from land, make buildings fall, and provide energy for whole countries.
In this Blink, you’ll learn how soft winds carry seeds, dust, and smoke far from where they began. You’ll see how simple science makes sunlight and air create big wind systems around the world. You’ll also learn how people have learned to use these winds for ships, mills, and today’s power systems. You will also find out how we measure wind, even though it never stops moving. And what happens when winds become very strong and dangerous.
To see where it all begins, it helps to start small, with the softest winds you barely notice.
Blink 1 – How the softest winds quietly reshape the world
On a bright morning in northern Wyoming, a mountain that was clear to see the day before suddenly vanished behind gray smoke. The air smelled of smoke. Local news said that fires in central Alberta, about a thousand miles away, had sent their ash south. Near the ground, the air hardly moved. But higher up, a steady wind had carried a clear stream of small bits through the lowest air layers. This is where most weather and pollution stay. Light winds, which are low on the Beaufort scale, can quietly change whole areas of land.
It is hard to believe how soft winds work unless you feel them. So, people have tried to describe them using human feelings. Lyall Watson, a scientist from South Africa, made a Biological Wind Scale. It starts with smoke going straight up from a chimney, then leaning a little. Then you feel the first touch of wind on your face. A little stronger, and fine dust starts to rise. Stronger still, and it hurts your eyes and makes walking hard. Even without tools, people and buildings show how strong the wind is. What looks still is actually air that is always moving and mixing.
Plants need this soft movement. Most plants cannot move, so their seeds must. The wind carrying seeds is one of their best tricks. Light seeds with soft, feather-like parts weigh almost nothing. The wind can carry them far from the tree they came from. Anyone can try this: put one hundred poplar seeds in a small bag. Place them on a special scale. The scale will hardly move. This shows how little the air needs to lift. Imagine thousands of seeds from one tree. Then you can see how light fluff can be carried by the wind across long distances.
Other plants try even harder each season. Maple and sycamore trees have stiff wings called samaras. These act like small spinning blades. They slow the seeds’ fall and let the wind push them sideways as they drop. On open flat lands, the way wind and plants work together can cause problems. In the late 1800s, Russian thistle seeds came to the Great Plains. They were mixed with flaxseed. In just a few decades, they had spread over large areas of land that had been moved. Each plant grows into a spiky ball. Then it breaks off. It rolls with the wind and drops hundreds of thousands of seeds. Today, these tumbleweeds pile up in dead-end streets and next to fences. They form big piles that block doors and roads. All this is caused by small winds that people hardly notice.
To understand how these small air movements get strong and take shape, let’s step back in the next section. We will ask where wind comes from and how it is set up around the whole planet.
Blink 2 – Wind starts when air meets heat that is not even
When the first astronauts landed on the moon in July 1969, people watching saw a flag that seemed to move in the wind. But the moon has almost no air, so there is no wind. Engineers had put a stiff bar along the top edge of the flag to make it look like it was waving. This trick shows the main rule for all wind: wind only happens when there is air to move and energy to make it move.
On Earth, that moving air is the atmosphere. It is a layer of gases around the planet, held in place by gravity. It is very heavy, about 5.5 quadrillion tons. It pushes on everything on Earth. Most weather and almost all daily winds happen in the lowest part, called the troposphere. This part goes up only a few miles. Above it is the stratosphere, which is much calmer.
The sun mainly provides the energy that moves this air layer. Our world is round. It tilts. It has land, water, ice, and clouds. Because of this, the sun’s light is not taken in evenly. Where the ground gets very warm, the air touching it gets bigger and lighter. Then it rises. This leaves an area with less air pressure. Cooler, heavier air from nearby then moves in to take its place. This sideways movement is wind in its simplest way.
If you look at this on a bigger scale, the same up-and-down movement creates a global wind system. It has three main bands in each half of the Earth. Near the equator, strong heat makes air rise. This air moves towards the poles high up, then sinks again near the subtropics. These wind loops are called Hadley cells. In the middle parts of the world, Ferrel cells connect that sinking air to the westerly winds on the ground. Near the poles, cold polar cells move heavy air away from the ice caps. Together, these cells create the trade winds near the equator, the westerlies in Europe and North America, and the jet streams. Jet streams run along the edges of these cells and guide big weather systems.
So, the air, the sun’s uneven heat, and the Earth’s spin work together. They create a three-cell system that forms the main winds around the world. These big wind patterns decide which coasts have warm winters. They decide which ocean paths are good for ships. And they decide which areas get stuck under very hot air or suffer from storms. When people understood these patterns, they started to see moving air as more than just daily weather. This is where the story of using wind to do work begins.
Blink 3 – Wind power becomes a tool for people to work
On a dry farm in the United States, a thin tower with a noisy wheel of metal blades can decide if a farm survives. Wind pumps on the plains, sold from the 1880s, use only moving air. They pull water from deep wells into large tanks. This keeps animals and families supplied in places that would otherwise be hard to live in.
Sailors learned to use this power at sea even earlier. Boats on the Nile River once could only go with the wind. But sailors learned to change sails and ropes. This let boats sail across the wind and even move against it. Later, in the time of big sailing ships, tall ships with square sails crossed oceans. They went around Cape Horn using large amounts of canvas. They moved goods and people along paths chosen for trade winds and westerly winds. They also knew about the calm areas where winds stopped.
In northern Europe, wind became like a hard-working helper on land. In the Netherlands, much land is at or below sea level. So, for hundreds of years, strong stone windmills with four long sails have pumped water from low lands and ground grain. Many still do this. Their gears change slow, strong turning into lifting water with pumps and spinning millstones. This helps create and protect farmland that would otherwise be swamp or sea. In America, the same idea led to many wooden and then steel wind pumps on the plains. Where the winds were steady, they were like a patient, free workforce.
In the late 1800s, people started trying to use wind to make electricity. In 1887, James Blyth, an engineer from Scotland, built a machine with cloth sails. It made electricity to charge batteries and light his house. Soon, similar machines were seen in North America and on windy coasts and islands. In the 1900s, these designs got bigger. They moved from small gardens to open hills and coastlines. In the 1970s, engineer William Heronemus from the University of Massachusetts helped create the design we know today: tall towers with three thin blades controlled by computers.
Today, this long process has created a system that uses wind for work. Hundreds of thousands of wind turbines now work around the world. Wind already provides more than half of Denmark’s electricity. It also provides a lot of power in countries like Germany and China. The same power that once filled big sails and shook wooden pumps now turns blades that are hundreds of feet long. It sends power into a country’s main electricity system.
When so much depends on moving air, it becomes even more important to say how strong it is. The next section will talk about the ways, numbers, and words we use to describe different winds.
Blink 4 – Measuring wind makes invisible air into numbers we can use
As wind began to power mills, move ships, and spin machines, people needed more than just a feeling about whether the day was windy or stormy. They wanted to know how fast the air was moving. They also wanted to compare wind in different places, even though wind cannot be seen and is always changing.
Early tries to measure wind were creative but not easy. Inventors hung flat pieces of metal on poles. The wind would tilt them against a scale. Or they timed runners who ran uphill with flags until their speed matched the wind’s speed. True progress came when Henri Pitot, a French engineer, worked in Paris in the 1700s. He showed that if liquid rose higher in a straight tube facing the wind, the wind was moving faster. This idea now helps pitot tubes work on most airplanes.
Later, Thomas Romney Robinson from Armagh worked hard to solve the puzzle of wind speed. At the city’s science center in the 1840s, he made a small machine. It had four empty cups on arms around a standing pole. When wind blows across the cups, the open parts feel more push than the round backs. This difference makes the whole cross turn. The faster the air moves, the faster the cups spin. Gears in the base change this movement into a number you can read on a dial. Engineers from that time already had tables showing how much wind pushes different shapes. This helped Robinson connect cup speed to wind speed very well. Today, types of his wind-measuring machine, called an anemometer, are still on poles and roofs everywhere.
But numbers don’t always show how wind feels. This is where Francis Beaufort comes in. He was a navy officer. He was annoyed by unclear words about weather in ship logs. So he made a scale that described what the wind did to the sea and sails at different strengths. It went from very calm to a big storm. Over time, the Beaufort scale became standard with twelve levels. Navies and weather services used it. It changed hard-to-describe winds into common pictures of small waves, white waves, and crashing waves. It is still used in the Shipping Forecast, which is broadcast every night around the British Isles. It uses numbers that show how the sea looks and acts.
Together, Robinson’s machine and Beaufort’s words show that even with careful design and categories, wind can only be measured roughly. This challenge is even more important in the last section. There, you’ll see how destructive winds change land and lives.
Blink 5 – Very strong winds show how easily societies can be hurt
In May 1934, New Yorkers started the day in spring sunshine. But they ended it under a dark sky. For five hours, Manhattan was half-dark. Car lights and streetlights were on at midday. Dust covered the streets and windows. It came from grasslands 1,500 miles away. This dust was part of 200 million tons of rich soil. The wind was lifting it from the Missouri and Mississippi valleys and pushing it east. This showed a small part of the disaster on the Great Plains.
On those plains, the same winds created walls of soil that covered the horizon. They pushed the soil into dunes up to nine feet deep. These dunes buried fences and houses almost to their roofs. The air in front of a dust storm could have so much static electricity that car engines stopped. Farm animals died from hunger and could not breathe. The land was so eroded that it looked like gravel. Families watched their farms disappear in the wind. Then they left in lines of old cars, looking for a place where the ground was safe.
Elsewhere, other places have learned to live with regular storms. They gave them names and built things to suit them. In southern France, the cold Mistral wind often rushes down the Rhône valley. So, farmhouses are built with their backs to the wind. Bell towers are made of open metalwork so the wind can pass through. The longest times of this wind are said to cause stress and sadness. Six hundred miles away in Trieste, the Bora wind rushes down from the Dinaric Alps. It is a very cold, strong wind. It is strong enough to flip cars and make people slide across the stone streets. Ropes were once tied along streets so weak people could cross without being blown away.
Nearer the equator, wind forms into small, strong spirals. Just before Christmas 1974, a tropical storm in the Arafura Sea got stronger and moved towards Darwin, in northern Australia. Early on Christmas Day, wind gusts hit 217 kilometers per hour. Then the measuring tools stopped working. By morning, about 90 percent of the city’s houses were destroyed. Tens of thousands of people were flown out in an emergency. Later, a new Darwin was planned and built, made to be stronger against storms.
These kinds of events help us understand why Admiral Samuel J. Locklear III gave a warning in 2013. He was in charge of over 300,000 US workers in the Indo-Pacific region. He said that rising sea levels, people forced to move, and stronger storms due to climate change could be a bigger long-term danger than other countries. The same moving air that can carry seeds, turn mills, and spin wind turbines is also changing where people live. And it is forcing them to start new lives in new places.
Final summary
The main idea from this Blink about The Breath of the Gods by Simon Winchester is this: the air around you plays a big part in nature and human history. Moving air connects far-off places and events. This happens with light poplar seeds, rolling tumbleweeds, fast jet streams, and dust clouds that make cities dark at midday. You can see these connections once you know what to look for. The same science that destroys houses and removes soil from fields also cools homes, fills sails, pumps water, and moves electricity along power lines. As the world gets warmer and winds change, understanding them helps you understand your future. It also reminds us that even something you cannot touch, like air, can become a strong helper if we are careful and clever.
Okay, that’s it for this Blink. We hope you enjoyed it. If you can, please take the time to leave us a rating – we always appreciate your feedback. See you in the next Blink.
Source: https://www.blinkist.com/https://www.blinkist.com/en/books/the-breath-of-the-gods-en