In October the World Meteorological Organization (WMO) released their report for worldwide water resources for 2023. The year 2023 marked the driest year for global rivers in over three decades, signaling critical changes in water availability in an era of growing demand.
The Key messages of the report:
- 2023
was driest year for global rivers in 33 years
- Glaciers
suffer largest mass loss in 50 years
- Climate
change appears to be making the hydrological cycle more erratic
- WMO highlights
that only north America and Europe (and a few other places like Israel)
have extensive monitoring networks that share data. WMO calls for better
monitoring and data sharing.
WMP report that the last five years have had widespread
below-normal conditions for river flows, and subsequently reservoir inflows have
also been below normal. This reduces the amount of water available for
communities, hydropower, agriculture and ecosystems, further stressing global
water supplies, according to the State
of Global Water Resources report.
Glaciers suffered the largest mass loss ever registered in
the last five decades. 2023 is the second consecutive year in which all regions
in the world with glaciers reported ice loss.
With 2023 being the hottest year on record (until 2024 data
is in), elevated temperatures and widespread dry conditions contributed to
prolonged droughts. But there were also a significant number of floods around
the world. The extreme hydrological events were influenced by naturally
occurring climate conditions – the transition from La Niña to El Niño in
mid-2023 – as well as human induced climate change.
from State of Global Water Resources report. |
“Water is the canary in the coalmine of climate change. We receive distress signals in the form of increasingly extreme rainfall, floods and droughts which wreak a heavy toll on lives, ecosystems and economies. Melting ice and glaciers threaten long-term water security for many millions of people. And yet we are not taking the necessary urgent action,” said WMO Secretary-General Celeste Saulo.
“As a result of rising temperatures, the hydrological cycle
has accelerated. It has also become more erratic and unpredictable, and we are
facing growing problems of either too much or too little water. A warmer
atmosphere holds more moisture which is conducive to heavy rainfall. More rapid
evaporation and drying of soils worsen drought conditions,” she said.
“And yet, far too little is known about the true state of
the world’s freshwater resources. We cannot manage what we do not measure. This
report seeks to contribute to improved monitoring, data-sharing, cross-border
collaboration and assessments,” said Celeste Saulo. “This is urgently needed.”
The State of Global Water Resources report series offers a
comprehensive and consistent overview of what we know of water resources worldwide. It is based
on input from dozens of National Meteorological and Hydrological Services and
other organizations and experts. This was the third year for the State of the
Global Water Resources report, and is
the most comprehensive to date, with new information on lake and reservoir
volumes, soil moisture data, and more details on glaciers and snow water
equivalent. So much more needs to be done.
Because some of the most available monitoring data is from
North America and Europe those areas had more detailed information and insight.
North America, for instance, was affected by the 2020–2023 North American
drought, but is also subject to groundwater depletion, in particular in
California and in the High Plains. The average groundwater level in 2023 was
below normal or much below normal in a high proportion of wells over a large
part of North America, in particular in the western and midwestern United
States,
High precipitation directly contributes to an increase in
groundwater levels through the recharge of aquifers. High precipitation also
tends to reduce groundwater abstraction, as more surface water is available,
less irrigation (or lawn watering) is necessary and the soil moisture is
higher, which indirectly contributes to an increase in groundwater levels.
Data were collected over the period covering the last
20 years, from 2004 to 2023. It is
not straightforward to identify the reasons behind these regional trends,
because groundwater is under the influence of climatic variables and other
anthropogenic variables, such as abstraction and land use/ land cover changes. Some aquifers have a
rapid response time between the change in the boundary conditions (such as a
groundwater recharge) and the corresponding change in groundwater level,
however the response time in other aquifers can be several years or decades
long. It is difficult to utilize general observations with this type of time
lag to for policy and manage resources. Nonetheless, it needs to be done.
Currently, 3.6 billion people face inadequate access to water at least a month per year and this is expected to increase to more than 5 billion by 2050, according to UN Water. We do not have enough monitoring here in the United States to adequately understand and manage our water resources. We are merely responsive to shortages not proactive. The Prince William County Board of Supervisors recently took the first step locally.
At the request of the Sustainability Commission, the Prince
William Board of County Supervisors (Board) accepted the Sustainability
Commission Resolution Number (Res. No.) 24-013 to direct County staff to assess
the sustainability of the County’s groundwater supply related to climate
change, urbanization, and other stressors.
Public Works staff worked with the United States Geological
Survey (USGS) and Virginia Tech’s Occoquan Watershed Monitoring Laboratory
(VT/OWML) to develop the scope of the study. A joint proposal was received from
the USGS and VT/OWML with a total cost of $480,000, the request for $500,000
includes any contingency costs that may arise above this cost proposal.
In November, the Prince William Board of County Supervisors voted to transfer - $500,000 from Contingency to the Department of Public Works for a countywide Groundwater Study.
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