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The Conversation
The Conversation
Environment
Pep Canadell, Chief research scientist, Climate Science Centre, CSIRO Oceans and Atmosphere; and Executive Director, Global Carbon Project, CSIRO

New research: nitrous oxide emissions 300 times more powerful than CO₂ are jeopardising Earth's future

Shutterstock

Nitrous oxide from agriculture and other sources is accumulating in the atmosphere so quickly it puts Earth on track for a dangerous 3℃ warming this century, our new research has found.

Each year, more than 100 million tonnes of nitrogen are spread on crops in the form of synthetic fertiliser. The same amount again is put onto pastures and crops in manure from livestock.

This colossal amount of nitrogen makes crops and pastures grow more abundantly. But it also releases nitrous oxide (N₂O), a greenhouse gas.

Agriculture is the main cause of the increasing concentrations, and is likely to remain so this century. N₂O emissions from agriculture and industry can be reduced, and we must take urgent action if we hope to stabilise Earth’s climate.

2000 years of atmospheric nitrous oxide concentrations. Observations taken from ice cores and atmosphere. Source: BoM/CSIRO/AAD.

Where does nitrous oxide come from?

We found that N₂O emissions from natural sources, such as soils and oceans, have not changed much in recent decades. But emissions from human sources have increased rapidly.

Atmospheric concentrations of N₂O reached 331 parts per billion in 2018, 22% above levels around the year 1750, before the industrial era began.

Agriculture caused almost 70% of global N₂O emissions in the decade to 2016. The emissions are created through microbial processes in soils. The use of nitrogen in synthetic fertilisers and manure is a key driver of this process.

Other human sources of N₂O include the chemical industry, waste water and the burning of fossil fuels.


Read more: Intensive farming is eating up the Australian continent – but there's another way


N₂O is destroyed in the upper atmosphere, primarily by solar radiation. But humans are emitting N₂O faster than it’s being destroyed, so it’s accumulating in the atmosphere.

N₂O both depletes the ozone layer and contributes to global warming.

As a greenhouse gas, N₂O has 300 times the warming potential of carbon dioxide (CO₂) and stays in the atmosphere for an average 116 years. It’s the third most important greenhouse gas after CO₂ (which lasts up to thousands of years in the atmosphere) and methane.

N₂O depletes the ozone layer when it interacts with ozone gas in the stratosphere. Other ozone-depleting substances, such as chemicals containing chlorine and bromine, have been banned under the United Nations Montreal Protocol. N₂O is not banned under the protocol, although the Paris Agreement seeks to reduce its concentrations.

A farmer emptying fertiliser into machinery
Reducing fertiliser use on farms is critical to reducing N₂O emissions. Shutterstock

What we found

The Intergovernmental Panel on Climate Change has developed scenarios for the future, outlining the different pathways the world could take on emission reduction by 2100. Our research found N₂O concentrations have begun to exceed the levels predicted across all scenarios.

The current concentrations are in line with a global average temperature increase of well above 3℃ this century.

We found that global human-caused N₂O emissions have grown by 30% over the past three decades. Emissions from agriculture mostly came from synthetic nitrogen fertiliser used in East Asia, Europe, South Asia and North America. Emissions from Africa and South America are dominated by emissions from livestock manure.

In terms of emissions growth, the highest contributions come from emerging economies – particularly Brazil, China, and India – where crop production and livestock numbers have increased rapidly in recent decades.

N₂O emissions from Australia have been stable over the past decade. Increase in emissions from agriculture and waste have been offset by a decline in emissions from industry and fossil fuels.

Regional changes in N₂O emissions from human activities, from 1980 to 2016, in million tons of nitrogen per year. Data from: Tian et al. 2020, Nature. Source: Global Carbon Project & International Nitrogen Initiative.

What to do?

N₂O must be part of efforts to reduce greenhouse gas emissions, and there is already work being done. Since the late 1990s, for example, efforts to reduce emissions from the chemicals industry have been successful, particularly in the production of nylon, in the United States, Europe and Japan.

Reducing emissions from agriculture is more difficult – food production must be maintained and there is no simple alternative to nitrogen fertilisers. But some options do exist.


Read more: Emissions of methane – a greenhouse gas far more potent than carbon dioxide – are rising dangerously


In Europe over the past two decades, N₂O emissions have fallen as agricultural productivity increased. This was largely achieved through government policies to reduce pollution in waterways and drinking water, which encouraged more efficient fertiliser use.

Other ways to reduce N₂O emissions from agriculture include:

  • better management of animal manure

  • applying fertiliser in a way that better matches the needs of growing plants

  • alternating crops to include those that produce their own nitrogen, such as legumes, to reduce the need for fertiliser

  • enhanced efficiency fertilisers that lower N₂O production.

Global nitrous oxide budget 2007-16. Adopted from Tian et al. 2020. Nature. Source: Global Carbon Project & International Nitrogen Initiative.

Getting to net-zero emissions

Stopping the overuse of nitrogen fertilisers is not just good for the climate. It can also reduce water pollution and increase farm profitability.

Even with the right agricultural policies and actions, synthetic and manure fertilisers will be needed. To bring the sector to net-zero greenhouse gas emissions, as needed to stabilise the climate, new technologies will be required.


Read more: Earth may temporarily pass dangerous 1.5℃ warming limit by 2024, major new report says


The Conversation

Pep Canadell receives funding from The Australian National Environmental Science Program, and the Gordon and Betty Moore Foundation.

Eric Davidson receives funding from the U.S. Department of Agriculture.

Glen Peters receives funding from the European Commission (Horizon 2020) and the Research Council of Norway.

Hanqin Tian receives funding from US National Science Foundation, National Oceanic and Atmospheric Administration, National Aeronautics and Space Administration and Andrew Carnegie Fellowship Program.

Michael Prather is an employee of the University of California at Irvine; currently has received research funding from NASA, NSF, US DOE, and private donors; and is a consultant for the Citizens Climate Lobby.

Paul Krummel is employed by CSIRO and receives funding from MIT, NASA, Australian Bureau of Meteorology, Department of Agriculture, Water and the Environment, and Refrigerant Reclaim Australia.

Rob Jackson receives funding from the Gordon and Betty Moore Foundation.

Rona Thompson receives funding from the European Commission (Horizon 2020) and the Research Council of Norway.

Wilfried Winiwarter currently receives funding from the Austrian national foundations for science (FWF) and applied research (FFG), from the Polish national foundation for applied research (NCBiR), and from UNEP via the Global Environment Fund.

This article was originally published on The Conversation. Read the original article.

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