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Phragmites Adaptive Management Framework: Model Overview
Phragmites Adaptive Management Framework: Model Overview
Phragmites Adaptive Management Framework: Model Overview

This animation is the third video in a series explaining different aspects of the Phragmites Adaptive Management Framework (PAMF). This video focuses on the machine learning model that PAMF uses to systematically learn from participant's data and then provide site-specific management guidance in return.

This animation is the third video in a series explaining different aspects of the Phragmites Adaptive Management Framework (PAMF). This video focuses on the machine learning model that PAMF uses to systematically learn from participant's data and then provide site-specific management guidance in return.

Photo of a calm creek with a small sandbar in the middle, creek is surrounded by trees burned by a wildfire.
Whiskey Creek section of Whiskeytown Lake
Whiskey Creek section of Whiskeytown Lake
Whiskey Creek section of Whiskeytown Lake

In the aftermath of the 2018 Carr Fire, northern California, sediment has eroded from burned hillslopes and accumulated in some areas of Whiskeytown Lake. A recent sediment deposit is shown here in the Whiskey Creek section of the lake.

In the aftermath of the 2018 Carr Fire, northern California, sediment has eroded from burned hillslopes and accumulated in some areas of Whiskeytown Lake. A recent sediment deposit is shown here in the Whiskey Creek section of the lake.

image related to volcanoes. See description
Zooming in even closer, an HVO scientist captured this image of the water on the
Zooming in even closer, an HVO scientist captured this image of the water on the
Zooming in even closer, an HVO scientist captured this image of the water on the

Zooming in even closer, an HVO scientist captured this image of the water on the floor of the crater during today's overflight. For more information, please read "Water or no water: that is (or was) the question"—HVO's Aug.

Zooming in even closer, an HVO scientist captured this image of the water on the floor of the crater during today's overflight. For more information, please read "Water or no water: that is (or was) the question"—HVO's Aug.

Cistern Spring, Yellowstone National Park, both full and drained
Cistern Spring, Yellowstone National Park, both full and drained
Cistern Spring, Yellowstone National Park, both full and drained
Cistern Spring, Yellowstone National Park, both full and drained

Photographs of Cistern Spring showing the draining behavior that occurs after major water eruptions of Steamboat Geyser. Left: about 2.5 hours after the onset of a major Steamboat eruption. Right: about 19.5 hours after that eruption.

Photographs of Cistern Spring showing the draining behavior that occurs after major water eruptions of Steamboat Geyser. Left: about 2.5 hours after the onset of a major Steamboat eruption. Right: about 19.5 hours after that eruption.

Doppler Radar Mounted On A Drone for Stream Velocity
Doppler Radar Mounted On A Drone for Stream Velocity
Doppler Radar Mounted On A Drone for Stream Velocity
Doppler Radar Mounted On A Drone for Stream Velocity

The sensor mounted on the drone is called the Qcam and is a Doppler radar sensor providing velocity from a hovering position above the river. USGS hydrologic technician (left) aboard a USGS John Boat mounted with Acoustic Doppler Current Profiler observes the Qcam conducting a measurement.

The sensor mounted on the drone is called the Qcam and is a Doppler radar sensor providing velocity from a hovering position above the river. USGS hydrologic technician (left) aboard a USGS John Boat mounted with Acoustic Doppler Current Profiler observes the Qcam conducting a measurement.

field crews of Hawaiian Volcano Observatory
field crews of Hawaiian Volcano Observatory
field crews of Hawaiian Volcano Observatory
field crews of Hawaiian Volcano Observatory

Kīlauea Volcano’s 2018 lower East Rift Zone eruption was monitored around the clock by field crews of Hawaiian Volcano Observatory and other USGS scientists for three months, starting with the first fissure that erupted in Leilani Estates on May 3, 2018.

Kīlauea Volcano’s 2018 lower East Rift Zone eruption was monitored around the clock by field crews of Hawaiian Volcano Observatory and other USGS scientists for three months, starting with the first fissure that erupted in Leilani Estates on May 3, 2018.

USGS LSPIV and Photogrametry Drones
USGS LSPIV and Photogrametry Drones
USGS LSPIV and Photogrametry Drones
USGS LSPIV and Photogrametry Drones

(Left) Frank Engel of the hydrologic remote sensing branch prepares the DJI Mavic Pro quadcopter , while Sean Andrews and Jeff Kinsey of the New England WSC observe. The Mavic was used for Large Scale Particle Image Velocimetry (LSPIV).

(Left) Frank Engel of the hydrologic remote sensing branch prepares the DJI Mavic Pro quadcopter , while Sean Andrews and Jeff Kinsey of the New England WSC observe. The Mavic was used for Large Scale Particle Image Velocimetry (LSPIV).

Photo of drone with ground-penetrating radar system flying close over river surface
USGS Tests drone-based ground-penetrating radar for bathymetry
USGS Tests drone-based ground-penetrating radar for bathymetry
USGS Tests drone-based ground-penetrating radar for bathymetry

USGS hydrographers collect tens of thousands of streamflow measurements every year. In-water work by personnel is one of the most dangerous aspects of USGS hydrologic studies, especially during high-flow conditions. In May 2019, USGS continued testing of a light-weight, self-contained ground-penetrating radar (GPR) system that can be mounted on a small drone.

USGS hydrographers collect tens of thousands of streamflow measurements every year. In-water work by personnel is one of the most dangerous aspects of USGS hydrologic studies, especially during high-flow conditions. In May 2019, USGS continued testing of a light-weight, self-contained ground-penetrating radar (GPR) system that can be mounted on a small drone.

USGS Tests Prototype Ground Penetrating Radar Drone
USGS Tests Prototype Ground Penetrating Radar Drone
USGS Tests Prototype Ground Penetrating Radar Drone
USGS Tests Prototype Ground Penetrating Radar Drone

The USGS, in cooperative research and development with GuidelineGEO, tested an 80 GHz self contained ground penetrating radar unit on a DJI Matrice 600 hexcopter (left). This platform was tested for flight performance and for measurement of river channel cross-sectional area as well as river water depth and river width.

The USGS, in cooperative research and development with GuidelineGEO, tested an 80 GHz self contained ground penetrating radar unit on a DJI Matrice 600 hexcopter (left). This platform was tested for flight performance and for measurement of river channel cross-sectional area as well as river water depth and river width.

USGS Water Science Center Personnel Conducting Measurements
USGS Water Science Center Personnel Conducting Measurements
USGS Water Science Center Personnel Conducting Measurements
USGS Water Science Center Personnel Conducting Measurements

(Above) New England Water Science Center and Virginia - West Virginia Water Science Center personnel collected measurements use GPS surveying equipment and ADCP to collect ground-truth data and quality assure non-contact data (above left Tom and Andy Massey; above right Andy Massey and Jeff Kinsey; lower left Russ Lotspeich on shore and Jeff Kinsey and Sean Andrews

(Above) New England Water Science Center and Virginia - West Virginia Water Science Center personnel collected measurements use GPS surveying equipment and ADCP to collect ground-truth data and quality assure non-contact data (above left Tom and Andy Massey; above right Andy Massey and Jeff Kinsey; lower left Russ Lotspeich on shore and Jeff Kinsey and Sean Andrews

Brachiopods in the Devonian Mahantango Formation
Brachiopods in the Devonian Mahantango Formation
Brachiopods in the Devonian Mahantango Formation
Brachiopods in the Devonian Mahantango Formation

NER May 2019 Where We Work
Brachiopods in the Devonian Mahantango Formation examined by Mercer Parker under the hand lens

Implanting an Acoustic Transmitter into a Cisco
Implanting an Acoustic Transmitter into a Cisco
Implanting an Acoustic Transmitter into a Cisco
Implanting an Acoustic Transmitter into a Cisco

Cisco being prepared for surgical implantation of an acoustic transmitter at the USGS Ann Arbor aquatic research laboratory

Cisco being prepared for surgical implantation of an acoustic transmitter at the USGS Ann Arbor aquatic research laboratory

Ripple marks in a bedding plane exposure of Devonian Foreknobs Formation
Ripple marks in a bedding plane exposure of Devonian Foreknobs
Ripple marks in a bedding plane exposure of Devonian Foreknobs
Ripple marks in a bedding plane exposure of Devonian Foreknobs

NER May 2019 Honorable Mention 2
Yvonne Dinh and Mercer Parker examine ripple marks in a bedding plane exposure of Devonian Foreknobs Formation

Photo of boat docks now surrounded by sand as the Salton Sea receeds.
Boat Docks High and Dry at the Salton Sea
Boat Docks High and Dry at the Salton Sea
Boat Docks High and Dry at the Salton Sea

As the Salton Sea continues to evaporate, old boat docks are now surrounded by sand and salt.

As the Salton Sea continues to evaporate, old boat docks are now surrounded by sand and salt.

Timelapse sequence shows a typical day at Mauna Loa's summit
Timelapse sequence shows a typical day at Mauna Loa's summit
Timelapse sequence shows a typical day at Mauna Loa's summit

This timelapse sequence of webcam images over a 24-hour period shows a typical day at the summit of Mauna Loa. The webcam (MLcam) is located on the northeast rim of Moku‘āweoweo, Mauna Loa's summit caldera. This sequence begins in the dark, with the moon rising (white dot at left in images), then brightens as the sun rises.

This timelapse sequence of webcam images over a 24-hour period shows a typical day at the summit of Mauna Loa. The webcam (MLcam) is located on the northeast rim of Moku‘āweoweo, Mauna Loa's summit caldera. This sequence begins in the dark, with the moon rising (white dot at left in images), then brightens as the sun rises.

Canning River with bars
Canning River with bars
Canning River with bars
Canning River with bars

Supporting the project of winter habitat of juvenile Dolly Varden in the Canning River.

Supporting the project of winter habitat of juvenile Dolly Varden in the Canning River.

Hole in the ice from an auger
Hole in the ice from an auger on Canning River
Hole in the ice from an auger on Canning River
Hole in the ice from an auger on Canning River

Supporting the project of winter habitat of juvenile Dolly Varden in the Canning River.

Interior mudflat on Jim Foot Key covered with saline water. Dead mangrove stumps and underwater grasses can be seen.
Interior Mudflat on Jim Foot Key, Florida
Interior Mudflat on Jim Foot Key, Florida
Interior Mudflat on Jim Foot Key, Florida

In Photo: Interior mudflat on Jim Foot Key covered with saline water, April 2019.  Stumps of dead mangroves (reportedly damaged by Hurricane Donna in 1960 (Craighead, 1962)) are visible projecting from the water.  Shadowed areas below the water are underwater grasses typically found in Florida Bay, now growing inside

In Photo: Interior mudflat on Jim Foot Key covered with saline water, April 2019.  Stumps of dead mangroves (reportedly damaged by Hurricane Donna in 1960 (Craighead, 1962)) are visible projecting from the water.  Shadowed areas below the water are underwater grasses typically found in Florida Bay, now growing inside

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