Hypoxia volumes in the Chesapeake Bay mainstem, spanning Maryland and Virginia, peaked above average in early summer 2025 before declining to below-average levels by late August and September, according to data from the Maryland Department of Natural Resources and Old Dominion University.
The monitoring program, which tracks dissolved oxygen in Bay waters from May through October, revealed early August volumes of 1.85 cubic miles of hypoxic water — defined as less than 2 milligrams per liter of oxygen — ranking as the 29th highest out of 38 years analyzed. Anoxia, waters with less than 0.2 milligrams per liter of oxygen, measured 0.54 cubic miles, more than double the long-term average. Conditions improved markedly thereafter, with late August hypoxia at 0.89 cubic miles, just below the 1.06-cubic-mile average, and anoxia dropping to 0.06 cubic miles, one-third of typical levels. By September, hypoxia fell to 0.21 cubic miles, less than half the 0.45-cubic-mile average, with no anoxia detected, though mechanical issues during the Sept. 15-17 cruise left some data gaps near the Maryland-Virginia line.

The seasonal shift aligned with weather patterns that initially fueled nutrient runoff into the Bay. Freshwater inflows preceding summer stood 20 percent above average, carrying excess nitrogen and phosphorus from agricultural fields, urban areas and wastewater sources. These nutrients trigger algal blooms, whose decomposition consumes oxygen and creates hypoxic zones, often called dead zones, that stress aquatic species.
May 2025 brought record rainfall to the region, with Maryland recording 7.81 inches, the highest total in 131 years tracked by NOAA’s National Centers for Environmental Information. Pennsylvania saw 7.72 inches, the second-wettest May on record. This deluge, coupled with June’s fourth-highest average temperature of 74.8 degrees and July’s second-highest of 79.9 degrees — both since 1895 — amplified runoff and bloom activity. Late June hypoxia reached 1.76 cubic miles, the 26th highest of 35 years, while early July hit 2.29 cubic miles, the 35th highest of 40 years. August cooled to 71.8 degrees, the 25th lowest since 1895, and brought drier conditions, with precipitation ranking seventh lowest in Maryland and third lowest in Pennsylvania, aiding oxygen recovery.
Scientists assess these volumes to gauge risks to Bay ecosystems, where hypoxia limits habitat for fish, crabs and oysters. In Southern Maryland’s lower Bay tributaries, such as the Patuxent and Potomac rivers, low-oxygen events can displace blue crabs — a key commercial species yielding over 20 percent of the state’s harvest — and hinder juvenile oyster growth in restoration sites like Harris Creek in Talbot County. Prolonged exposure forces mobile species like menhaden and striped bass to shallower, warmer waters, increasing vulnerability to predators and disease. Immobile bottom-dwellers, including worms and clams, face mortality rates up to 90 percent in severe anoxic pockets.
The Chesapeake Bay Program, a federal-state partnership since 1983, coordinates pollution reduction strategies targeting a 2025 goal of cutting nitrogen loads by 29 percent from 2009 levels. Progress includes upgrades to wastewater treatment plants, which removed 1.2 million pounds of nitrogen in 2024, and cover crops on 1.1 million acres of farmland to curb runoff. Maryland’s 2025 nutrient trading program, expanded under the Water Quality Improvement Act, incentivizes farmers to adopt precision fertilization, reducing phosphorus by an estimated 15 percent in the Patuxent watershed. These measures, funded partly by the EPA’s $90 million annual allocation, have shrunk average annual hypoxia by 12 percent since 1985, though climate variability like 2025’s extremes underscores ongoing challenges.
Monitoring involves biweekly cruises by DNR vessels, sampling 30 stations along the mainstem from Pooles Island near Baltimore to the Bay mouth. Teams deploy a CTD profiler to measure oxygen, salinity and temperature at depths up to 174 feet, with data processed via geospatial models to calculate volumes. Virginia’s Department of Environmental Quality contributes parallel surveys, and the EPA supports analysis through Old Dominion’s Center for Coastal Resources Management. Results feed into Eyes on the Bay, an online dashboard updated monthly with maps and trends dating to 1984.
Early season data reflected this variability: May showed no hypoxia, tying for the best of 41 years. Early June’s 0.68 cubic miles ranked 13th of 37, and late July’s 1.74 cubic miles placed 24th of 40. The full 2025 summary, relative to 1985-2024 averages, appears below:
2025 Cruise Hypoxic Volume Average Volume (1985-2024) 2025 Rank Graphic May 0.0 0.19 1st (tied) / 41 Chart or Map Early June 0.68 0.85 13th / 37 Chart or Map Late June 1.76 1.25 26th / 35 Chart or Map Early July 2.29 1.59 35th / 40 Chart or Map Late July 1.74 1.62 24th / 40 Chart or Map Early August 1.85 1.29 29th / 38 Chart or Map Late August 0.89 1.06 18th / 41 Chart or Map September 0.21 0.45 10th / 41 Chart or Map
Ranks indicate lower numbers as better water quality.
As fall progresses, cooler temperatures and reduced stratification should sustain improvements, though tropical storm remnants could introduce new nutrients. DNR plans October cruises to close the season, with preliminary findings expected in November. Residents can access real-time data via Eyes on the Bay to track conditions in local waters, informing decisions on fishing and crabbing in areas like Point Lookout or Solomons Island.
The Bay’s hypoxia issue traces to colonial-era land clearing, but intensified post-World War II with fertilizer use surging 400 percent. The 1987 Chesapeake Bay Agreement marked a turning point, committing signatories to restoration. By 2025, over 5,000 miles of riparian buffers along streams have filtered pollutants, benefiting Southern Maryland’s 1,200 miles of shoreline. Yet, with sea levels rising 1 foot since 1900 and projections of 2 feet by 2050, adaptive strategies like wetland expansion in Calvert County aim to buffer future extremes.
