A continued record-breaking ocean temperature with increasing in stratification and changes in water salinity pattern give insight into what the future holds amidst a perpetually heating climate.
The state of our oceans can measure the world’s health, and judging by the updated oceanic observations from 24 scientists across 16 institutes worldwide, we need a doctor. The three key indicators of climate change include continued historical record-breaking temperatures, all-time high levels of ocean salinity-contrast, and increased ocean stratification (separation of the water into layers) with no signs of slowing down. These indicators are leading scientists to quickly address and forecast future components of climate change to better prepare the public for an extreme climate future ahead.
Results were recently published where a new record of 0-2000m ocean heat content (OHC) was set and recorded in 2022, with an addition of approximately ~10 Zetta joules (ZJ) of heat into the ocean than 2021. A Zetta joule is a joule (unit to measure “work” or “heat”) with 21 zeros behind it.
The results were published on 11 January 2023 in Advances in Atmospheric Science. It summarizes two international datasets: from the Institute of Atmospheric Physics (IAP) at the Chinese Academy of Sciences (CAS), and from the National Centers for Environmental Information (NCEI) of the National Oceanic and Atmospheric Administration (NOAA), that analyze observations of ocean heat content and their impact dating from the 1950s. “Both IAP and NCEI data show a consistent message that upper 2000m ocean heat content hits a record high value in 2022”, said Tim Boyer, a senior researcher from NCEI/NOAA.
10 ZJ of heat is equal to ~100 times world electricity generation in 2021 (28466 TWH), ~325 times China’ 2021 electricity production (8537 TWH), ~634 times United States’ 2021 electricity production (4381 TWH). 10 ZJ of heat can also boil 700 million 1.5L kettle for every second in the past year.
“Global warming continues and is manifested in record ocean heat, and also in continued extremes of salinity. The latter highlight that salty areas get saltier, and fresh areas get fresher and so there is a continuing increase in intensity of the hydrological cycle” said Lijing Cheng, lead author and researcher for the IAP/CAS.
What's not hard to grasp is how that amount of heat going into the oceans have serious consequences, and actually comes much quicker than one would hope. The increasing saltiness and therefore stratification of the oceans can alter how heat, carbon, and oxygen are exchanged between the ocean and the atmosphere above it. This is a factor that can cause ocean deoxygenation, or loss of oxygen, within the water. Deoxygenation itself is a nightmare for not only marine life and ecosystems but also for humans and our terrestrial ecosystems.
Reducing oceanic diversity and displacing important species can wreak havoc on fishing-dependent communities and their economies, and this can have a ripple effect on the way most people are able to interact with their environment.
Some places are already seeing the impacts of a rapidly warming ocean, and they're not exactly as expected.
“Some places are experiencing more droughts, which lead to an increased risk of wildfires, and other places are experiencing massive floods from heavy rainfall, often supported by increased evaporation from warm oceans. This contributes to changes in the hydrologic cycle and emphasizes the interactive role that oceans play.” said Kevin Trenberth, third author of the paper and researcher at both the National Center for Atmospheric Research and the University of Auckland. An increase in water temperatures and salinity directly contributes to water layering instead of mixing, and this is just part of what throws off the delicate balance between our oceans and the atmosphere.
“In the future, the group will focus on understanding the changes of the earth’s major cycles and improve the future projections of earth’s heat, water and carbon changes. This is the basis for human[s] to prepare for the future changes and risks” said John Abraham, Professor of University of St. Thomas, the second author of this study.
Continued tracking of these changes will give scientists an idea of what can be done preemptively to prepare for higher temperatures, extreme weather, and all other consequences that come along with warming oceans and an impacted hydrologic cycle.
“The oceans are absorbing most of the heating from human carbon emissions,” said paper author Michael Mann, Professor of University of Pennsylvania. “Until we reach net zero emissions, that heating will continue, and we’ll continue to break ocean heat content records, as we did this year. Better awareness and understanding of the oceans are a basis for the actions to combat climate change.”
Advances in Atmospheric Sciences
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