A new study of ocean salinity finds substantial amplification of the global water cycle

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A new study of ocean salinity finds substantial amplification of the global water cycle

An illustration of global water cycle and its change. Credit: Figure adapted from NASA (gpm.nasa.gov/education/water-cycle)

 

Water and its movements within or between atmosphere, land and ocean defines the global water cycle and is central to the climate system. Almost all

 

weather and climate phenomena are in some way tied to the water cycle. Examples include extreme rainfall during thunderstorms, hurricanes and

 

tropical cyclones, flooding, droughts, and sea level rise.

 

Now, the water cycle is changing in important ways as the climate changes. Theory and models suggest that as the Earth is warming, the global water

 

cycle is amplified, i.e., more water is evaporated from the ocean, and consequently, precipitation is increasing, as well. Yet the observational

 

confirmation of this prediction has been difficult, since past changes of the water cycle are were poorly observed due to the difficulty of measuring

 

global-scale evaporation and precipitation and the complexity of their spatial and temporal variability.

 

The new study, published in the Journal of Climate, overcomes many of the previous limitations and derives a new estimate of water cycle change based

 

on salinity data since 1960. From this, they provided strong new evidence that the global water cycle has amplified substantially in the past 50 years,

 

confirming theory and models. The study is led by Lijing Cheng from the Institute of Atmospheric at the Chinese Academy of Sciences, who collaborated

 

with a group of international scientists from National Center for Atmospheric Research, U.S.; ETH Zurich; University of St. Thomas, U.S.; Pennsylvania

 

State University, U.S.

 

0-2000 mean salinity climatology (top) shows the relatively fresh Pacific versus the salty Atlantic northern Indian Ocean. Its long-term trend (middle) has a remarkably similar pattern. The zonal mean ocean salinity trends (bottom) since 1960 in each ocean basin, organized around the Southern Ocean in the center, depict the penetration of surface anomalies into the ocean subsurface. Credit: Lijing Cheng

 

"Ocean salinity change can be used to estimate water cycle change because it reveals the modification of global surface freshwater exchanges:

 

Evaporation takes freshwater from the ocean into the atmosphere and increases the ocean salinity; precipitation puts more freshwater into the ocean

 

and reduces the salinity. Consequently, salinity changes integrate effects over broad areas and provide an excellent indicator for water cycle change,"

 

said Lijing Cheng.

 

"However, as previous salinity datasets show severe biases or shortcomings, we needed better salinity data. This study provides new monthly gridded

 

salinity fields for the upper 2000 meters since 1960," John Abraham said. "To perform interpolation across data sparse intervals and regions, the

 

method uses information on the spatio-temporal co-variability of salinity taken from the historical coupled climate model simulations. The method is

 

then rigorously verified."

 

"The new product is clearly more reliable for examining long-term salinity changes, as we show that this new salinity reconstruction has much better

 

continuity through changes in the observing-system (from altimeters on satellites and profiling floats (Argo) in the ocean," said co-author Kevin

 

Trenberth from NCAR. "The new data demonstrate that the existing salinity pattern has amplified. In other words, 'the fresh gets fresher, and the salty

 

gets saltier' in much of the ocean. Also, we show, for the first time, that the averaged salinity trend of the ocean zero-to-2000-meter depth indicates

 

freshening in almost the entire Pacific Ocean, broad salinification in the low- and middle-latitudes Atlantic, pronounced freshening in North Atlantic,

 

and contrasts between the north and south Indian ocean."

 

Salinity-contrast time series from 1960 to 2017 at upper 2000m. Credit: Background Photograph: Xilin Wang.

 

The salinity change is spatially complicated. This study uses a simple index to synthesize these changes, named the salinity contrast (SC) index, which is

 

defined as the difference between the salinity averaged over high-salinity and low-salinity regions. "This metric provides a simple but powerful means

 

of synthesizing the observed salinity pattern changes," said Nicolas Gruber, a coauthor of this study from ETH. "We show that the zero-to-2000-meter

 

salinity pattern has amplified by 1.6% and surface salinity has amplified by 7.5%. We also show that this increase is due to human influence, and this

 

anthropogenic signal has exceeded the natural background variability."

 

An improved estimate of the global water cycle change has been compiled based on the new salinity data, salinity-contrast metrics and model

 

simulations. It shows that the water cycle has been already amplified by 2 to 4 % per degree Celsius since 1960 (Figure 1). "Our ocean-based result is

 

broadly consistent with many recent atmospheric based estimates and strengthens the evidence that the global water cycle has been intensified with

 

global warming," said John Fasullo from NCAR, U.S.

 

This result has important implications for the future climate. In a world warmed by +2°C (the upper limit of the Paris Agreement target), the water cycle

 

will amplify by 4~8%. This amplification will be even stronger if the aerosol impacts are smaller in the future than today (i.e., if the air pollution can be

 

controlled). Consequently, there will be stronger evaporation: The drier regions will get even drier and further increase the odds of worsening drought.

 

Droughts affect livestock and crops and increase risk of sometimes deadly wildfire in many regions, including the U.S., China, Australia, Brazil and other

 

countries, posing severe risks to food safety and human health. There will also be greatly increased risk of heavy and extreme rains. The more intense

 

rainstorms cause major problems like extreme flooding around the world. The rainfall associated with tropical cyclones and hurricanes will continue to

 

grow and increase damage not only to coastal and small island communities, but inland as well (as in Hurricane Isaias).

 

"This study is a significant advance in the field," said Michael Mann from Pennsylvania State University, U.S.: "First, the new, more accurate estimates of

 

salinity changes provide a better basis for comparison with climate model simulations. Secondly, the salinity-contrast index provides a key measure of

 

climate change impact on the global water hydrological cycle and helps distinguish the signal. We find that it takes a little more than a decade to isolate

 

the climate change signal from background noise in this particular metric, suggesting it should be used more widely by the climate research

 

community."

 

 

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