Join the Celebration!

   

Celebrating 100 Years of Science! | 1925-2025

  • UMCES HOME
  • DONATE

Search form

  • Work with Us
    • Science communication services
    • Environmental report card production
    • Training and capacity building
    • Stakeholder Engagement
    • Careers
  • Media Library
    • Symbols
    • Graphics
    • Photos
    • Videos
  • Report cards
  • Education
    • Professional Certificate
    • MEES Graduate Program
    • Short Courses
    • Initiatives
  • Blog
  • Enewsletter
  • Publications
    • Books
    • Report Cards
    • Newsletters
    • Reports
    • Brochures
    • Posters
    • Papers
  • Projects
  • About
    • Who we are
    • What we do
    • Our Mission
    • History
    • Partnerships
    • Contact
    • Land Acknowledgment Statement
    • Project Videos
  • Home
  • Media Library
Clear Filters

Lightbox (0)

Symbol Package
Impervious surfaces like roofs and parking lots cannot absorb water. A large volume of rainfall in a relatively short period of time produces runoff, which carries sediments and chemicals into bodies of water. Storm drains cannot always handle the volume of water, or get backed up for other reasons, creating puddles like this one in a parking lot. Video taken in Arnold, Maryland.
Stormwater runoff
Coastal flooding that occurs on sun, storm-free days can be caused by unusually high tides. Offshore storms can contribute to these tides, but are not always the cause. During these events, coastal storm drains can back up and flood streets and walkways. Video taken in Eastport, Annapolis, Maryland.
Tidal or nuisance flooding
During heavy rainfall, water runs off impervious surfaces like sidewalks. Manmade or paved surfaces like roofs and roads cannot absorb water like vegetated surfaces, so rainwater flows directly into the nearest body of water, carrying sediments and other pollutants with it.
Runoff in action
A short timelapse of the sun rising over the choptank river
Sunrise over the Choptank Timelapse
Timelapse of clouds rolling over large bay area.
Cloud Timelapse
Icon representing a cold front.
Cold Front
Wind
Weather: wind 3
Illustration of clouds with rain falling down
Weather: rain 2
Illustration of wind flow
Weather: wind 2
A conceptual diagram shows the process between pressure, response, and state during a large storm.
Pressure response diagram
This diagram illustrates the main threats from hurricanes and tropical storms. The counterclockwise circulation of winds in the Northern Hemisphere causes maximum winds and maximum storm surges.
Threats from Hurricanes and Tropical Storms
The Chesapeake Bay watershed received an above average annual amount of precipitation in 2013. This accompanied degrading conditions in some regions of the Chesapeake Bay watershed and improving conditions in others.
Chesapeake Bay Watershed Percipitation Map 2013
Diagram depicting Human-caused and natural vulnerabilities of Chesapeake Bay to climate impacts.
Human-caused and natural vulnerabilities of…
Conceptual diagram illustrating how hurricanes are structured and formed.
Hurricane formation
Conceptual diagram illustrating south Florida, located along the southern margin of the temperate region of North America and the northern margin of the tropics.
South Florida climate zone
Conceptual diagram illustrating wet season (left) and dry season (right) variations in south Florida weather patterns.
South Florida weather patterns
summer high humidity hangs suspended over soybean field
summer humidity over soybean field
waterspout rises over a local river
Waterspout
Illustration of the Pleiades constellation.
Constellation: Pleiades
Illustration of a waning gibbous moon.
Moon
Rain storm approaches rural community of Neavitt, Maryland.
Storm clouds threaten
Illustration of the sun, symbolizing solar radiation (energy from the sun)
Weather: solar radiation
Illustration of a cloud blowing air symbolizing wind
Weather: wind 1
Illustration of a wind vector, the two- or three-dimensional vector describing the instantaneous wind magnitude and direction at a point (often using Cartesian coordinates; i.e. X and Y wind vectors). The term can also apply to the resultant wind vector which is sometimes drawn as an arrow with length proportional to wind speed.
Weather: wind vector
  • 1
  • 2
  • 3
  • Next

UMCES Links

  • Home
  • About
  • Campuses
  • News & Events
  • Directory
  • Employment
  • Research
  • Press Room

Contact Info

2020 Horns Point Rd
Cambridge, MD 21613

410-221-2048

Contact

Enewsletter

Subscribe to our enewsletter

Copyright 2025 UMCES | Privacy/Terms of Use | An Institution of the University System of Maryland