EOPS_December_31_2016,
The year 2016 in pictures: After two years of very warm air and record high water temperatures starting with the Blob (2015) and followed by El Nino (2016), temperatures have fallen and remain slightly warmer than normal in Puget Sound. Very low summer river flows (e.g., Fraser River) reflect climatic predictions for the NW. Record temperatures and low salinities occurred alongside observations of abundant jellyfish, floating macro-algae, and Noctiluca blooms. Surprisingly, only South Sound developed very low summer oxygen levels in 2016. In the fall, La Niña came with a punch, rain increased, and air temperatures dropped. Will this be an unusual La Niña?
Publication No. 16-03-079
EOPS_May_2_2016,
Spring air temperatures are higher - it has been sunny and dry. The snowpack is quickly disappearing as temperatures are up to 7 °F warmer at higher elevations. Snowmelt-fed rivers are running very high. How does this affect water quality in Puget Sound? A strong spring phytoplankton bloom extends across Puget Sound and the Strait of Juan de Fuca. Water temperatures are still higher than normal and jellyfish are already numerous in southern inlets. The high biological activity is causing organic material to drift at the surface and wash onto beaches. Do you know how fast a Sand Star can move?
Ecology Publication No. 16-03-073
EOPS_June_27_2016,
Record-breaking warmer and fresher water in Puget Sound. May-June conditions are more unusual than last year. Recent rain brought river flows close to normal but water exchange in Puget Sound remains weak due to low Fraser River flow. Phytoplankton blooms and organic material are visible in some areas of Central and South Sound but not in others. Noctiluca, while absent in Central Basin, was reported in unusual places. Jelly fish occur only in some south sound bays. Follow our BEACH program kick off, discover the Stinkworm, and find good underwater visibility for diving.
Ecology Publication No. 16-03-074
EOPS_April_6_2016,
Despite warmer air temperatures, normal snowpack in the mountains suggest that summer freshwater flows into Puget Sound might be higher than last year. As of April, the spring plankton bloom has extended across Central and South Puget Sound. Ferry data shows chlorophyll increasing after March 25 and expanding across the area. With water temperatures above normal as a carry-over from 2015, jellyfish patches are numerous in inlets of South Sound and in Sinclair Inlet, unusual for this time of year. Check out the tiny burrowing ostracods as well as our Washington Conservation Corps Intern analyzing seawater oxygen.
Ecology Publication No. 16-03-072
The document provides observations from aerial photos taken on September 16, 2014, noting numerous and large patches of jellyfish seen in the finger inlets of South Sound and East Sound near Orcas Island, as well as red-brown blooms remaining strong in smaller bays inside Puget Sound, with suspended sediment from the Nooksack and Skagit Rivers also visible. Water quality conditions including water temperature, salinity, and dissolved oxygen levels are discussed for different regions of Puget Sound based on long-term monitoring data. Climate and oceanic conditions that influence Puget Sound waters are also reviewed.
EOPS_March_16_2016,
In response to warm and wet conditions, rivers have been running high. Salinity in Puget Sound is notably lower. Below a cooler surface, water temperatures remain high, especially in Hood Canal. We still see numerous jellyfish patches in Puget Sound inlets. Phytoplankton blooms are going strong in Hood Canal and Henderson Inlet, and picking up elsewhere. Many places showed long stretches of suspended sediments nearshore, a sign of potential shore erosion. Check out the critters inhabiting the sediments of Puget Sound.
Ecology Publication No. 16-03-071
Warm air and water temperatures and offshore winds have persisted since fall. Numerous and sizable jelly fish patches are still present in southern inlets of Puget Sound. Coastal waters were colored in shades of gray to brown by sediment and humic substances. Phytoplankton blooms were restricted to the surf zone. We were treated to artful views of meandering sloughs and gullies on exposed mud flats during low tide in Willapa Bay, interspersed with the geometry of shellfish management. Brown pelicans: a story of recovery.
EOPS_September_26_2016,
September is jellyfish season and they are everywhere in southern Puget Sound! Sunny, warm, and dry conditions promoted strong late-summer plankton blooms in colors of red, green, and brown, now widespread in many bays. In contrast, Central Sound looks clear with low algal activity. Southern Puget Sound has large floating mats of organic material and developed lower oxygen in August. Meet the Critter of the Month - The Sweet Potato Sea Cucumber.
Publication No. 16-03-077
Sunshine and warm temperatures return after last week’s intense rain. The Puyallup and Nisqually Rivers are flowing high. Red-brown blooms and numerous patches of jellyfish remain strong in South Sound, Sinclair and Dyes Inlets, and Bellingham Bay, with brown-green blooms in Whidbey Basin. Macro-algae surface debris is very high in South and Central Sound. Hood Canal remains cooler but Puget Sound-wide temperatures are now warmer and less salty. Sea surface temperatures are above 15 °C, conditions favorable for some pathogens, and harmful algae blooms. Read about super colonies of by-the-wind sailors washing up on our shores.
EOPS_May_2_2016,
Spring air temperatures are higher - it has been sunny and dry. The snowpack is quickly disappearing as temperatures are up to 7 °F warmer at higher elevations. Snowmelt-fed rivers are running very high. How does this affect water quality in Puget Sound? A strong spring phytoplankton bloom extends across Puget Sound and the Strait of Juan de Fuca. Water temperatures are still higher than normal and jellyfish are already numerous in southern inlets. The high biological activity is causing organic material to drift at the surface and wash onto beaches. Do you know how fast a Sand Star can move?
Ecology Publication No. 16-03-073
EOPS_June_27_2016,
Record-breaking warmer and fresher water in Puget Sound. May-June conditions are more unusual than last year. Recent rain brought river flows close to normal but water exchange in Puget Sound remains weak due to low Fraser River flow. Phytoplankton blooms and organic material are visible in some areas of Central and South Sound but not in others. Noctiluca, while absent in Central Basin, was reported in unusual places. Jelly fish occur only in some south sound bays. Follow our BEACH program kick off, discover the Stinkworm, and find good underwater visibility for diving.
Ecology Publication No. 16-03-074
EOPS_April_6_2016,
Despite warmer air temperatures, normal snowpack in the mountains suggest that summer freshwater flows into Puget Sound might be higher than last year. As of April, the spring plankton bloom has extended across Central and South Puget Sound. Ferry data shows chlorophyll increasing after March 25 and expanding across the area. With water temperatures above normal as a carry-over from 2015, jellyfish patches are numerous in inlets of South Sound and in Sinclair Inlet, unusual for this time of year. Check out the tiny burrowing ostracods as well as our Washington Conservation Corps Intern analyzing seawater oxygen.
Ecology Publication No. 16-03-072
The document provides observations from aerial photos taken on September 16, 2014, noting numerous and large patches of jellyfish seen in the finger inlets of South Sound and East Sound near Orcas Island, as well as red-brown blooms remaining strong in smaller bays inside Puget Sound, with suspended sediment from the Nooksack and Skagit Rivers also visible. Water quality conditions including water temperature, salinity, and dissolved oxygen levels are discussed for different regions of Puget Sound based on long-term monitoring data. Climate and oceanic conditions that influence Puget Sound waters are also reviewed.
EOPS_March_16_2016,
In response to warm and wet conditions, rivers have been running high. Salinity in Puget Sound is notably lower. Below a cooler surface, water temperatures remain high, especially in Hood Canal. We still see numerous jellyfish patches in Puget Sound inlets. Phytoplankton blooms are going strong in Hood Canal and Henderson Inlet, and picking up elsewhere. Many places showed long stretches of suspended sediments nearshore, a sign of potential shore erosion. Check out the critters inhabiting the sediments of Puget Sound.
Ecology Publication No. 16-03-071
Warm air and water temperatures and offshore winds have persisted since fall. Numerous and sizable jelly fish patches are still present in southern inlets of Puget Sound. Coastal waters were colored in shades of gray to brown by sediment and humic substances. Phytoplankton blooms were restricted to the surf zone. We were treated to artful views of meandering sloughs and gullies on exposed mud flats during low tide in Willapa Bay, interspersed with the geometry of shellfish management. Brown pelicans: a story of recovery.
EOPS_September_26_2016,
September is jellyfish season and they are everywhere in southern Puget Sound! Sunny, warm, and dry conditions promoted strong late-summer plankton blooms in colors of red, green, and brown, now widespread in many bays. In contrast, Central Sound looks clear with low algal activity. Southern Puget Sound has large floating mats of organic material and developed lower oxygen in August. Meet the Critter of the Month - The Sweet Potato Sea Cucumber.
Publication No. 16-03-077
Sunshine and warm temperatures return after last week’s intense rain. The Puyallup and Nisqually Rivers are flowing high. Red-brown blooms and numerous patches of jellyfish remain strong in South Sound, Sinclair and Dyes Inlets, and Bellingham Bay, with brown-green blooms in Whidbey Basin. Macro-algae surface debris is very high in South and Central Sound. Hood Canal remains cooler but Puget Sound-wide temperatures are now warmer and less salty. Sea surface temperatures are above 15 °C, conditions favorable for some pathogens, and harmful algae blooms. Read about super colonies of by-the-wind sailors washing up on our shores.
The document provides a surface conditions report for Puget Sound on November 22, 2016, summarizing the climate, water quality measurements, aerial photographs, continuous monitoring data, and streamflow levels. Aerial photographs show large jellyfish aggregations in the inlets of South Puget Sound and fading algal blooms in Eld and Budd Inlets. Water temperatures and salinities have mostly returned to normal levels following record highs, though Hood Canal and South Sound are still warmer than typical.
Unusually warm water temperatures continue in central and south Puget Sound. River flows remain lower than normal, especially the Fraser and Skagit rivers. Thus, with estuarine circulation much weaker, Puget Sound waters stay put. Mats of organic debris persist in Central Sound near Port Madison. Red-brown and brown blooms are now very strong in southern inlets and jellyfish patches are exceptionally numerous and large. Explore media coverage of unusual Puget Sound conditions including jellyfish.
The document summarizes conditions in Puget Sound related to warm water anomalies, drought, and impacts on marine ecosystems. It notes that 2014 and early 2015 saw the warmest temperatures since 1981 due to a warm water blob in the Pacific. This, combined with low snowpack due to drought, led to record low river flows into Puget Sound. The warm water entered Puget Sound in late 2014 and 2015, bringing higher temperatures and lower oxygen levels. Observations from aerial photos and ferries detected large jellyfish blooms and algal blooms, indicating the marine food web may be changing.
Puget Sound is starting to normalize in response to fall conditions with cooler air temperatures, rain, and recovering river flows. We are seeing fewer algal blooms, jellyfish, and macro-algae as salinities become more normal. Yet warm waters persist and El Nino and the Blob are likely to affect Puget Sound throughout the winter. The Nisqually River fared better through the drought than other rivers and best management practices have been improving its water quality. EOPS and ferry monitoring gain recognition with a national award for innovation!
Air temperatures are warm and Puget Sound continues to show record high water temperatures. Some rain has returned to our region, yet river flows remain unusually low. Puget Sound is saltier than normal allowing oxygen-rich surface waters to more easily mix to greater depths. Lower oxygen was measured only in the Coastal Bays, Hood Canal, and South Sound. Large jellyfish aggregations continue in South Sound, the Kitsap Peninsula, and East Sound (Orcas Island). Sediment plumes in Bellingham Bay form unique patterns. Warm waters and sunny conditions fostered green tides, raising a stink along some local beaches.
The aerial photos from June 23, 2014 showed the following:
- Large mats of surface debris were seen in Hood Canal, Padilla Bay, Lay Inlet and parts of Georgia Basin. Many of the patches contained macro-algae.
- A strong red-brown phytoplankton bloom was observed in Discovery Bay, East Sound and parts of Georgia Basin.
- The water north of the San Juan Islands appeared sediment-rich.
- Jellyfish numbers seemed to be increasing in locations like Budd Inlet and Hood Canal.
A stunning view of a second large Noctiluca bloom captures the attention of many living near Puget Sound. Favorable conditions support several regional phytoplankton blooms. Red-brown blooms in Port Townsend, Discovery Bay and Bellingham Bay. Large algal mats or organic material particularly in Samish Bay. Jellyfish patches increasing in Budd, Totten and Eld Inlets.
EOPS_July_24_2017,
July had warm air temperatures, sunshine, and an abundant snowpack. Previous months had higher river flows (bringing freshwater) and weak upwelling (low delivery of saltier water) which resulted in very low salinities in Puget Sound, especially in the South Sound. Water temperatures are expected and warmer in Central Sound. Above normal sunshine has made Puget Sound biologically very active! Intense and unusual blooms color Hood Canal (coccolithophores) and south sound inlets. Large mats of organic material containing macro-algae drift at the surface. Many schools of fish are visible though jellyfish were absent.
Ecology Publication No. 17-03-071
EOPS_December_30_2015,
The year 2015 in pictures: Jellyfish patches persisted through the entire year in response to the exceptionally warm water caused by the Blob. Sediment loads are high as snow melts fast in the winter of 2015. Unexpected phytoplankton species occur in some bays in spring. Noctiluca, jellyfish and macro-algae appear in high numbers when rivers drop to record-low flows in early summer. Low river flows slow the renewal of in Puget Sound throughout summer and fall and jellyfish patches reach record highs.
Ecology Publication No. 15-03-080
EOPS_July_20_2016,
Through June, air temperatures and sunlight were higher than normal. Recent rain generally improved river flows. However, the Fraser river flow remains extremely low, reducing water exchange with the ocean. Water temperatures are still breaking records, yet dissolved oxygen levels are normal. Coastal bays are influenced by upwelling and exhibit lower oxygen and higher salinities. Puget Sound algae are thriving with blooms observed in many South Sound inlets. Macro-algae is seen piling up on beaches and drifting in Central Sound. Jellyfish smacks are numerous in Eld and Budd Inlets. Our fliers notice seals hanging out at the beach!
Ecology Publication No. 16-03-075
The ocean and air remain warm with sunshine and dry weather across the region. As a result, Puget Sound is a lot warmer going into the new year. Hood Canal is responding with temperatures warmer than previous measurements, breaking its low temperature stint. First signs of growing phytoplankton are coloring the water green. Patches of jellyfish are overwintering in finger inlets of South Sound. Tidal fronts and suspended sediment are visible amidst the stunning San Juan Islands scenery. A sediment-rich water mass is trapped in Rosario Strait. Check out the South Sound Estuarium and the many reasons we love Puget Sound!
EOPS_June_5_2017,
Cooler and wetter conditions early in 2017 have set the stage for a favorable supply of freshwater. River flows are all above normal due to melting of the abundant snowpack from warmer May air temperatures. This is creating significantly fresher conditions in Puget Sound surface waters. Algae blooms are limited to some yellow-green blooms growing in bays near the Kitsap Peninsula and blooms near estuaries of the Skagit, Stillaguamish, and Puyallup Rivers. Red blooms are present in rivers feeding into Willapa Bay. Also see what is “blooming” in the sediments of Puget Sound.
Ecology Publication No. 17-03-070
Unusually warm water temperatures continue in central and south Puget Sound while Willapa Bay returns to expected water temperatures as a result of stronger coastal upwelling. Extensive mats of organic debris develop in many places, particularly in Central Sound overlapping with a fading Noctiluca bloom. King County confirms Noctiluca and shares plankton species information. Red-brown and brown blooms are going strong in southern inlets and around the San Juan Islands. Our inspiring WCC Intern gets on boats, into the air, and to the lab.
A stunning view of a second large Noctiluca bloom captures the attention of many living near Puget Sound. Favorable conditions support several regional phytoplankton blooms. Red-brown blooms in Port Townsend, Discovery Bay and Bellingham Bay. Large algal mats or organic material particularly in Samish Bay. Jellyfish patches increasing in Budd, Totten and Eld Inlets.
1) Aerial photography on April 21, 2014 showed blooms in Whidbey Basin and isolated bays, with otherwise clear water. Sediment-rich water was entering Puget Sound from the Stillaguamish River after the Oso mudslide. Debris lines were observed in Hood Canal and North Sound. Multiple oil sheens were seen in the Lake Washington Ship Canal.
2) Physical conditions in Puget Sound were developing into colder, saltier conditions throughout the region. Dissolved oxygen levels were lower in Whidbey Basin, Central Sound, and South Sound but higher in Hood Canal.
3) Upwelling conditions off the Washington coast in mid-April stimulated a spring phytop
EOPS_August_24_2016,
In July, conditions were normalizing, yet river flows remained lower, continuing into August. July also saw lower oxygen appearing in southern Puget Sound. By August, jellyfish are occurring in high numbers in Eld and Budd Inlet. South Puget Sound has Noctiluca drifting at the surface in large orange lines in many places and red-brown blooms widespread in finger inlets, as well as in Sinclair Inlet. Central Sound surface-water temperatures are high, still in the 60s, and algae are abundant. See what we are measuring to understand ocean acidification in Puget Sound.
Publication No. 16-03-076
Warmer and sunnier days result in higher than normal river flows from the Skagit and Nisqually. Biological activity in the water column is high. Abundant organic surface debris in Hood Canal, Padilla Bay, and many Inlets. Red-brown blooms in South Sound, Discovery Bay, and regions of Bellingham Bay. Different blooms in Skagit Bay, Padilla Bay, and Sinclair Inlet. Jelly fish are numerous in all southernmost South Sound Bays. Hood Canal remains cold but Puget Sound-wide temperatures are now warmer and less salty. Data from the Victoria Clipper and our sampling in the Strait provides important information on water exchange with the ocean.
EOPS_October_6_2015,
Puget Sound is starting to normalize in response to fall conditions with cooler air temperatures, rain, and recovering river flows. We are seeing fewer algal blooms, jellyfish, and macro-algae as salinities become more normal. Yet warm waters persist and El Nino and the Blob are likely to affect Puget Sound throughout the winter. The Nisqually River fared better through the drought than other rivers and best management practices have been improving its water quality. EOPS and ferry monitoring gain recognition with a national award for innovation!
Ecology Publication No. 15-03-078
At the end of summer, water temperatures are still high, and salinities and dissolved oxygen are low in Puget Sound. Both sea surface temperature and upwelling off the coast are elevated (PDO and Upwelling indices) and the the Fraser River flow is low. This combination makes it an interesting fall. Very dense and large patches of jellyfish appear in finger inlets of South Sound. Red-brown blooms also remain strong in South Sound.
The document provides an overview of marine conditions in Puget Sound and surrounding areas from aerial photos taken on October 29, 2014, noting very dense patches of jellyfish in the fingers inlets of South Sound, strong red-brown algal blooms remaining in smaller bays, and increasing visibility of suspended sediments; it also describes physical conditions like water temperature, salinity and dissolved oxygen levels based on long-term monitoring data and compares conditions to historical trends.
The weather changed from cool, cloudy and southerlies, to sunny warm conditions and light northerly winds on Mother’s Day. At the water surface, blooms and large debris lines occur in Bellingham, Padilla, and Samish Bays, Hood Canal, East Sound, and the Straits, as well as the finger inlets of South Sound. Large amounts of sediment-laden water from Port Susan are flowing into Central Basin. Turquoise water mixing to the surface in places around the San Juan Islands. After some trouble-shooting of the hardware and communication system, we will resume collecting Victoria Clipper data next week. Meet Eyes Under Puget Sound: Sediment Monitoring Program at Ecology.
The document provides a surface conditions report for Puget Sound on November 22, 2016, summarizing the climate, water quality measurements, aerial photographs, continuous monitoring data, and streamflow levels. Aerial photographs show large jellyfish aggregations in the inlets of South Puget Sound and fading algal blooms in Eld and Budd Inlets. Water temperatures and salinities have mostly returned to normal levels following record highs, though Hood Canal and South Sound are still warmer than typical.
Unusually warm water temperatures continue in central and south Puget Sound. River flows remain lower than normal, especially the Fraser and Skagit rivers. Thus, with estuarine circulation much weaker, Puget Sound waters stay put. Mats of organic debris persist in Central Sound near Port Madison. Red-brown and brown blooms are now very strong in southern inlets and jellyfish patches are exceptionally numerous and large. Explore media coverage of unusual Puget Sound conditions including jellyfish.
The document summarizes conditions in Puget Sound related to warm water anomalies, drought, and impacts on marine ecosystems. It notes that 2014 and early 2015 saw the warmest temperatures since 1981 due to a warm water blob in the Pacific. This, combined with low snowpack due to drought, led to record low river flows into Puget Sound. The warm water entered Puget Sound in late 2014 and 2015, bringing higher temperatures and lower oxygen levels. Observations from aerial photos and ferries detected large jellyfish blooms and algal blooms, indicating the marine food web may be changing.
Puget Sound is starting to normalize in response to fall conditions with cooler air temperatures, rain, and recovering river flows. We are seeing fewer algal blooms, jellyfish, and macro-algae as salinities become more normal. Yet warm waters persist and El Nino and the Blob are likely to affect Puget Sound throughout the winter. The Nisqually River fared better through the drought than other rivers and best management practices have been improving its water quality. EOPS and ferry monitoring gain recognition with a national award for innovation!
Air temperatures are warm and Puget Sound continues to show record high water temperatures. Some rain has returned to our region, yet river flows remain unusually low. Puget Sound is saltier than normal allowing oxygen-rich surface waters to more easily mix to greater depths. Lower oxygen was measured only in the Coastal Bays, Hood Canal, and South Sound. Large jellyfish aggregations continue in South Sound, the Kitsap Peninsula, and East Sound (Orcas Island). Sediment plumes in Bellingham Bay form unique patterns. Warm waters and sunny conditions fostered green tides, raising a stink along some local beaches.
The aerial photos from June 23, 2014 showed the following:
- Large mats of surface debris were seen in Hood Canal, Padilla Bay, Lay Inlet and parts of Georgia Basin. Many of the patches contained macro-algae.
- A strong red-brown phytoplankton bloom was observed in Discovery Bay, East Sound and parts of Georgia Basin.
- The water north of the San Juan Islands appeared sediment-rich.
- Jellyfish numbers seemed to be increasing in locations like Budd Inlet and Hood Canal.
A stunning view of a second large Noctiluca bloom captures the attention of many living near Puget Sound. Favorable conditions support several regional phytoplankton blooms. Red-brown blooms in Port Townsend, Discovery Bay and Bellingham Bay. Large algal mats or organic material particularly in Samish Bay. Jellyfish patches increasing in Budd, Totten and Eld Inlets.
EOPS_July_24_2017,
July had warm air temperatures, sunshine, and an abundant snowpack. Previous months had higher river flows (bringing freshwater) and weak upwelling (low delivery of saltier water) which resulted in very low salinities in Puget Sound, especially in the South Sound. Water temperatures are expected and warmer in Central Sound. Above normal sunshine has made Puget Sound biologically very active! Intense and unusual blooms color Hood Canal (coccolithophores) and south sound inlets. Large mats of organic material containing macro-algae drift at the surface. Many schools of fish are visible though jellyfish were absent.
Ecology Publication No. 17-03-071
EOPS_December_30_2015,
The year 2015 in pictures: Jellyfish patches persisted through the entire year in response to the exceptionally warm water caused by the Blob. Sediment loads are high as snow melts fast in the winter of 2015. Unexpected phytoplankton species occur in some bays in spring. Noctiluca, jellyfish and macro-algae appear in high numbers when rivers drop to record-low flows in early summer. Low river flows slow the renewal of in Puget Sound throughout summer and fall and jellyfish patches reach record highs.
Ecology Publication No. 15-03-080
EOPS_July_20_2016,
Through June, air temperatures and sunlight were higher than normal. Recent rain generally improved river flows. However, the Fraser river flow remains extremely low, reducing water exchange with the ocean. Water temperatures are still breaking records, yet dissolved oxygen levels are normal. Coastal bays are influenced by upwelling and exhibit lower oxygen and higher salinities. Puget Sound algae are thriving with blooms observed in many South Sound inlets. Macro-algae is seen piling up on beaches and drifting in Central Sound. Jellyfish smacks are numerous in Eld and Budd Inlets. Our fliers notice seals hanging out at the beach!
Ecology Publication No. 16-03-075
The ocean and air remain warm with sunshine and dry weather across the region. As a result, Puget Sound is a lot warmer going into the new year. Hood Canal is responding with temperatures warmer than previous measurements, breaking its low temperature stint. First signs of growing phytoplankton are coloring the water green. Patches of jellyfish are overwintering in finger inlets of South Sound. Tidal fronts and suspended sediment are visible amidst the stunning San Juan Islands scenery. A sediment-rich water mass is trapped in Rosario Strait. Check out the South Sound Estuarium and the many reasons we love Puget Sound!
EOPS_June_5_2017,
Cooler and wetter conditions early in 2017 have set the stage for a favorable supply of freshwater. River flows are all above normal due to melting of the abundant snowpack from warmer May air temperatures. This is creating significantly fresher conditions in Puget Sound surface waters. Algae blooms are limited to some yellow-green blooms growing in bays near the Kitsap Peninsula and blooms near estuaries of the Skagit, Stillaguamish, and Puyallup Rivers. Red blooms are present in rivers feeding into Willapa Bay. Also see what is “blooming” in the sediments of Puget Sound.
Ecology Publication No. 17-03-070
Unusually warm water temperatures continue in central and south Puget Sound while Willapa Bay returns to expected water temperatures as a result of stronger coastal upwelling. Extensive mats of organic debris develop in many places, particularly in Central Sound overlapping with a fading Noctiluca bloom. King County confirms Noctiluca and shares plankton species information. Red-brown and brown blooms are going strong in southern inlets and around the San Juan Islands. Our inspiring WCC Intern gets on boats, into the air, and to the lab.
A stunning view of a second large Noctiluca bloom captures the attention of many living near Puget Sound. Favorable conditions support several regional phytoplankton blooms. Red-brown blooms in Port Townsend, Discovery Bay and Bellingham Bay. Large algal mats or organic material particularly in Samish Bay. Jellyfish patches increasing in Budd, Totten and Eld Inlets.
1) Aerial photography on April 21, 2014 showed blooms in Whidbey Basin and isolated bays, with otherwise clear water. Sediment-rich water was entering Puget Sound from the Stillaguamish River after the Oso mudslide. Debris lines were observed in Hood Canal and North Sound. Multiple oil sheens were seen in the Lake Washington Ship Canal.
2) Physical conditions in Puget Sound were developing into colder, saltier conditions throughout the region. Dissolved oxygen levels were lower in Whidbey Basin, Central Sound, and South Sound but higher in Hood Canal.
3) Upwelling conditions off the Washington coast in mid-April stimulated a spring phytop
EOPS_August_24_2016,
In July, conditions were normalizing, yet river flows remained lower, continuing into August. July also saw lower oxygen appearing in southern Puget Sound. By August, jellyfish are occurring in high numbers in Eld and Budd Inlet. South Puget Sound has Noctiluca drifting at the surface in large orange lines in many places and red-brown blooms widespread in finger inlets, as well as in Sinclair Inlet. Central Sound surface-water temperatures are high, still in the 60s, and algae are abundant. See what we are measuring to understand ocean acidification in Puget Sound.
Publication No. 16-03-076
Warmer and sunnier days result in higher than normal river flows from the Skagit and Nisqually. Biological activity in the water column is high. Abundant organic surface debris in Hood Canal, Padilla Bay, and many Inlets. Red-brown blooms in South Sound, Discovery Bay, and regions of Bellingham Bay. Different blooms in Skagit Bay, Padilla Bay, and Sinclair Inlet. Jelly fish are numerous in all southernmost South Sound Bays. Hood Canal remains cold but Puget Sound-wide temperatures are now warmer and less salty. Data from the Victoria Clipper and our sampling in the Strait provides important information on water exchange with the ocean.
EOPS_October_6_2015,
Puget Sound is starting to normalize in response to fall conditions with cooler air temperatures, rain, and recovering river flows. We are seeing fewer algal blooms, jellyfish, and macro-algae as salinities become more normal. Yet warm waters persist and El Nino and the Blob are likely to affect Puget Sound throughout the winter. The Nisqually River fared better through the drought than other rivers and best management practices have been improving its water quality. EOPS and ferry monitoring gain recognition with a national award for innovation!
Ecology Publication No. 15-03-078
At the end of summer, water temperatures are still high, and salinities and dissolved oxygen are low in Puget Sound. Both sea surface temperature and upwelling off the coast are elevated (PDO and Upwelling indices) and the the Fraser River flow is low. This combination makes it an interesting fall. Very dense and large patches of jellyfish appear in finger inlets of South Sound. Red-brown blooms also remain strong in South Sound.
The document provides an overview of marine conditions in Puget Sound and surrounding areas from aerial photos taken on October 29, 2014, noting very dense patches of jellyfish in the fingers inlets of South Sound, strong red-brown algal blooms remaining in smaller bays, and increasing visibility of suspended sediments; it also describes physical conditions like water temperature, salinity and dissolved oxygen levels based on long-term monitoring data and compares conditions to historical trends.
The weather changed from cool, cloudy and southerlies, to sunny warm conditions and light northerly winds on Mother’s Day. At the water surface, blooms and large debris lines occur in Bellingham, Padilla, and Samish Bays, Hood Canal, East Sound, and the Straits, as well as the finger inlets of South Sound. Large amounts of sediment-laden water from Port Susan are flowing into Central Basin. Turquoise water mixing to the surface in places around the San Juan Islands. After some trouble-shooting of the hardware and communication system, we will resume collecting Victoria Clipper data next week. Meet Eyes Under Puget Sound: Sediment Monitoring Program at Ecology.
Sunshine and warmth continue into September. Upwelling is higher, yet low Fraser River flow reduces the likelihood of low-oxygen water moving into Puget Sound. Dissolved oxygen remains relatively high in Hood Canal and is lower elsewhere. Satellites show relatively warm water in the Strait of Georgia and Whidbey Basin and an extensive offshore bloom. Water temperatures also remain high in South Sound were red-brown plankton blooms and large smacks of jellyfish adorn the water surface. Explore what frequent blooms in smaller bays can tell us.
EOPS_August_28_2017,
Warm air temperatures, abundant sunshine, and drier conditions persisted. River flows are lower in the north. Puget Sound waters are still fresher than in the past 17 years from the combination of abundant spring rain and weak upwelling bringing less salty water from the ocean. July upwelling was stronger, however. Warmer water temperatures are notable in parts of Central Sound, accompanied by large rafts of drifting macroalgae. Diverse blooms in colors of green, orange and red-brown are present in many inlets. Jellyfish abundance is lower this year. Find out how we assess if the benthos is changing.
Ecology Publication No. 17-03-072
A stunning view of a second large Noctiluca bloom captures the attention of many living near Puget Sound. Favorable conditions support several regional phytoplankton blooms. Red-brown blooms in Port Townsend, Discovery Bay and Bellingham Bay. Large algal mats or organic material particularly in Samish Bay. Jellyfish patches increasing in Budd, Totten and Eld Inlets.
After a wet January, precipitation levels in March were near or below normal in the Puget Sound region. Snowpack levels were around 109% of normal, meaning streamflows feeding Puget Sound were expected to be normal or above normal through September. Water temperatures in Puget Sound in February were slightly above the long-term average, within ranges for herring spawning but approaching the minimum survival threshold for anchovies of 8°C. Early spring blooms were observed in the finger inlets of South Puget Sound as sunlight and conditions improved.
The year 2014 in pictures: In 2014, Puget Sound and Hood Canal behaved distinctly different in temperature and dissolved oxygen. In Puget Sound, generally warmer conditions, abundant and diverse algal blooms, and large pools of organic material persisted along with lower oxygen, high jellyfish abundances, and a lot of suspended sediment. On the other hand, Hood Canal was colder, more oxygenated, and algae blooms were rare. People and planes: past and present.
Warm waters from “The Blob” in Puget Sound combine with drought conditions as warm air has left little snow to feed the rivers. Water temperatures throughout Puget Sound are the highest in 25 years and oxygen is exhibiting record lows. High suspended sediment in the north is still coming in from the Fraser River. Otherwise, the surface waters appear very clear due to recent low river flows and weak blooming activity. A red bloom is present in Sinclair Inlet and in some confined bays. Patches of jellyfish, however, are going strong in inlets of South Sound and Sinclair Inlet. What does this all mean for salmon? Get to know some intertidal critters!
1) Jellyfish still aggregate in patches in South Puget Sound inlets. Early signs of increasing phytoplankton appear in coastal bays mixing with sediment-rich waters.
2) Winter precipitation has lowered salinity in Puget Sound significantly but temperatures remain at record highs, though cooler along the coast. Oxygen levels are mostly normal.
3) Continuous monitoring via ferry sensors shows near-surface water remains cool and mixed on ferry routes, with higher turbidity in the Strait of Juan de Fuca than Puget Sound. Early February saw increased colored dissolved organic matter in Whidbey Basin.
After a dry summer, precipitation levels increased in recent months but river flows remain lower than 2018. In October, surface water temperatures were slightly above average across Puget Sound. Optimal temperatures for species like anchovies and salmon persisted in some areas. Aerial photos from October 30th show sizable rafts of organic debris in many regions as well as some red-brown algal blooms, though many blooms had dissipated. Green water persisted in parts of South Sound.
Extensive red-brown algal blooms were observed in South Sound and Quartermaster Harbor from aerial flights and satellite imagery. Large patches of macroalgae were also seen throughout Central Sound. Dissolved oxygen levels began declining at some monitoring stations, while surface temperatures ranged from 14-15°C in Central Sound to 10-11°C in the Strait of Juan de Fuca. The latest algal bloom in Central Sound showed signs of fading as waters began to clear.
Improving the viability of probiotics by encapsulation methods for developmen...Open Access Research Paper
The popularity of functional foods among scientists and common people has been increasing day by day. Awareness and modernization make the consumer think better regarding food and nutrition. Now a day’s individual knows very well about the relation between food consumption and disease prevalence. Humans have a diversity of microbes in the gut that together form the gut microflora. Probiotics are the health-promoting live microbial cells improve host health through gut and brain connection and fighting against harmful bacteria. Bifidobacterium and Lactobacillus are the two bacterial genera which are considered to be probiotic. These good bacteria are facing challenges of viability. There are so many factors such as sensitivity to heat, pH, acidity, osmotic effect, mechanical shear, chemical components, freezing and storage time as well which affects the viability of probiotics in the dairy food matrix as well as in the gut. Multiple efforts have been done in the past and ongoing in present for these beneficial microbial population stability until their destination in the gut. One of a useful technique known as microencapsulation makes the probiotic effective in the diversified conditions and maintain these microbe’s community to the optimum level for achieving targeted benefits. Dairy products are found to be an ideal vehicle for probiotic incorporation. It has been seen that the encapsulated microbial cells show higher viability than the free cells in different processing and storage conditions as well as against bile salts in the gut. They make the food functional when incorporated, without affecting the product sensory characteristics.
RoHS stands for Restriction of Hazardous Substances, which is also known as t...vijaykumar292010
RoHS stands for Restriction of Hazardous Substances, which is also known as the Directive 2002/95/EC. It includes the restrictions for the use of certain hazardous substances in electrical and electronic equipment. RoHS is a WEEE (Waste of Electrical and Electronic Equipment).
Optimizing Post Remediation Groundwater Performance with Enhanced Microbiolog...Joshua Orris
Results of geophysics and pneumatic injection pilot tests during 2003 – 2007 yielded significant positive results for injection delivery design and contaminant mass treatment, resulting in permanent shut-down of an existing groundwater Pump & Treat system.
Accessible source areas were subsequently removed (2011) by soil excavation and treated with the placement of Emulsified Vegetable Oil EVO and zero-valent iron ZVI to accelerate treatment of impacted groundwater in overburden and weathered fractured bedrock. Post pilot test and post remediation groundwater monitoring has included analyses of CVOCs, organic fatty acids, dissolved gases and QuantArray® -Chlor to quantify key microorganisms (e.g., Dehalococcoides, Dehalobacter, etc.) and functional genes (e.g., vinyl chloride reductase, methane monooxygenase, etc.) to assess potential for reductive dechlorination and aerobic cometabolism of CVOCs.
In 2022, the first commercial application of MetaArray™ was performed at the site. MetaArray™ utilizes statistical analysis, such as principal component analysis and multivariate analysis to provide evidence that reductive dechlorination is active or even that it is slowing. This creates actionable data allowing users to save money by making important site management decisions earlier.
The results of the MetaArray™ analysis’ support vector machine (SVM) identified groundwater monitoring wells with a 80% confidence that were characterized as either Limited for Reductive Decholorination or had a High Reductive Reduction Dechlorination potential. The results of MetaArray™ will be used to further optimize the site’s post remediation monitoring program for monitored natural attenuation.
Evolving Lifecycles with High Resolution Site Characterization (HRSC) and 3-D...Joshua Orris
The incorporation of a 3DCSM and completion of HRSC provided a tool for enhanced, data-driven, decisions to support a change in remediation closure strategies. Currently, an approved pilot study has been obtained to shut-down the remediation systems (ISCO, P&T) and conduct a hydraulic study under non-pumping conditions. A separate micro-biological bench scale treatability study was competed that yielded positive results for an emerging innovative technology. As a result, a field pilot study has commenced with results expected in nine-twelve months. With the results of the hydraulic study, field pilot studies and an updated risk assessment leading site monitoring optimization cost lifecycle savings upwards of $15MM towards an alternatively evolved best available technology remediation closure strategy.
Kinetic studies on malachite green dye adsorption from aqueous solutions by A...Open Access Research Paper
Water polluted by dyestuffs compounds is a global threat to health and the environment; accordingly, we prepared a green novel sorbent chemical and Physical system from an algae, chitosan and chitosan nanoparticle and impregnated with algae with chitosan nanocomposite for the sorption of Malachite green dye from water. The algae with chitosan nanocomposite by a simple method and used as a recyclable and effective adsorbent for the removal of malachite green dye from aqueous solutions. Algae, chitosan, chitosan nanoparticle and algae with chitosan nanocomposite were characterized using different physicochemical methods. The functional groups and chemical compounds found in algae, chitosan, chitosan algae, chitosan nanoparticle, and chitosan nanoparticle with algae were identified using FTIR, SEM, and TGADTA/DTG techniques. The optimal adsorption conditions, different dosages, pH and Temperature the amount of algae with chitosan nanocomposite were determined. At optimized conditions and the batch equilibrium studies more than 99% of the dye was removed. The adsorption process data matched well kinetics showed that the reaction order for dye varied with pseudo-first order and pseudo-second order. Furthermore, the maximum adsorption capacity of the algae with chitosan nanocomposite toward malachite green dye reached as high as 15.5mg/g, respectively. Finally, multiple times reusing of algae with chitosan nanocomposite and removing dye from a real wastewater has made it a promising and attractive option for further practical applications.
BASIC CONCEPT OF ENVIRONMENT AND DIFFERENT CONSTITUTENET OF ENVIRONMENT
Eops 2016 12_31
1. Eyes Over Puget Sound
Up-to-date observations of visiblewater quality conditions in Puget Sound and the Strait of Juan de Fuca
Publication No. 16-03-079
2016
Review
La Niña, September 2016El Niño, January 2016
https://www.climate.gov/news-features/featured-images/september-2016-tropical-pacific-update
EOPS Weather Climate Species Respond Water column Aerial photos
2. Subscribe to our
dedicated email
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Join 670 users.
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Ecology scientists behind EOPS
Thanks to interested viewers,we are providing
information for a diverse audience
www.ecy.wa.gov/programs/eap/mar_wat/eops/Previous Eyes Over Puget Sound reports:
2016 – The EOPS team thanks all our viewers
Mya Keyzers
Laura Hermanson
Skip
Albertson
Dr. Christopher
Krembs
EOPS Weather Climate Species Respond Water column Aerial photos
GOV
29%
COM + NET
22%
EDU
25%
ORG
14%
US
8%
MIL
2%
outside US
0%
Tyler Burks
Don Watt
User demographics based on best guesses per e-mail extensions
Carol Maloy
Julianne Ruffner
Jim Shedd
Markus von Prause
Marine
Rivers andStreams Suzan Pool
Julia Bos
3. Climate and naturalinfluences,includingweather,rivers,and the adjacent ocean,can
affect our marine waters. Graphics are basedonprovisional dataandare subject to
change. http://www.ecy.wa.gov/programs/eap/mar_wat/weather.html,page 26.
Summary:
Air temperatures have dropped
sharply. The end of 2016 looks
like La Niña conditions.
Precipitation levels droppedfrom
November to December,whichis
atypical for La Niña.
Sunshine inDecember is close to
normal.
Riverflows in December are
fallingagainbelow normal in
response to low precipitation,
except for the Fraser River.
Downwelling (opposite of
upwelling) is weak in December,
followingtwo strongdownwelling
months (Oct and Nov). higher No datalowerexpected*Upwelling Anomalies (PFEL)
2016 – Weather in review for the last years
EOPS Weather Climate Species Respond Water column Aerial photos
20162015
5. Where do all the macro-algae endup after July? A lot of the material ends up on beaches.
2016 – Species indicating eutrophication
Algae washed up on beaches in thick layers and rotting.
Location:Edmonds Underwater Park, SnohomishCounty,July2016.
EOPS Weather Climate Species Respond Water column Aerial photos
6. Jellyfish and red-browndinoflagellate blooms thriving in warm, stagnantwaterin late summer.
2016 – Species indicating eutrophication
Two differently colored red-brown blooms and abundant jellyfishpatches.
Location:Budd Inlet (South Sound),September 2016.
EOPS Weather Climate Species Respond Water column Aerial photos
7. Noctiluca and organic material accumulating near Boston Harbor
Entrance to BuddInlet (South Sound),.
Noctilucathriving in eutrophic, stagnatingwaterin many places, May-August2016.
2016 – Species indicating at eutrophication
Noctiluca bloom, marine in Budd Inlet
Noctiluca bloom Pickering Passage,Case Inlet
EOPS Weather Climate Species Respond Water column Aerial photos
8. We usea boatand
chartered float plane to
access our monthly
monitoring stations most
costeffectively.
We communicate data and
environmentalmarine
conditions using:
1. Marine Water
Condition Index
(MWCI)
2. Eyes OverPuget
Sound (EOPS)
3. Anomaliesand
sourcedata
Ourlong-termmarinemonitoringstations
Starthere
San Juan Island
.
Stationsare sampled byregion.Both float
plane and boat are equippedwithsensors
and samplinggear (CTD)
EOPS Weather Climate Species Respond Water column Aerial photos
9. Much Warmer! Fresher to SaltierShifts. LowerDO.
Explore profiles
at all stations
Blob and El Niño affect Temperature Oxygen lower in summerSalinity follows rivers & rainfall
In2016 temperatures were stillremarkablyhigh in Puget Sound due to ElNiño conditions following
effects of the 2015 Blob event. Warmer temperatures bothyears forcedshifts inhydrology withmore
winter rainfall creatingfresher conditions while drought effects insummer led to higher than normal
salinity levels. In2016,oxygenlevels were lower thannormal,particularly in SouthSound.
EOPS Weather Climate Species Respond Water column Aerial photos
10. Feb.
Mar.
Apr.
May.
June
Jul.
Aug.
Sept.
Nov.
Snowpack declines in response to warm air from El Niño. Jellyfish patches prevail through
winter.
Rivers are flowing high, salinities are low, and water temperatures remain at record levels. First blooms appear and
jellyfish patches prevail. Strong rain brings sediment into Puget Sound.
Water is warm and fresher, the spring phytoplankton bloom spreads across Central and South Sound. Jellyfish
patches are very numerous. Herring are spawning.
Jellyfish occur in high numbers. The spring phytoplankton bloom is in full swing extending into the Straits. Organic
material is floating at the surface in large quantities, including Noctiluca. Record warm water continues.
Salinity is much lower than usual and temperatures are still at record highs. Oxygen is lower while drifting organic
material and Noctiluca appear at the surface on a large scale in unusual places.
River flows decrease. Macro-algae and other organic debris proliferate in large quantities at the surface where
water temperatures climb above 15°C. Conditions are ripe for HABS.
Red-brown blooms spread, jellyfish and Noctiluca thrive. July precipitation improves stream flows, while a drought
in B.C. impacts the Fraser River in the north, resulting in slower water renewal in the Salish Sea system.
Jellyfish patches reach very high densities. Red-brown blooms are abundant in South Sound and oxygen levels are
much lower. In contrast, algal abundance in Central Sound is low.
El Niño fades as wet and warm weather conditions prevail. Water temperatures finally return to normal after two
years. Salinities, oxygen, and stream flows are normalizing. Yet, jellyfish are abundant in South Sound.
Jellyfish patches persisted with continued record warmtemperatures. Noctiluca, jellyfish, and
macro-algaeoccurred in high numbers. The Fraser River dropped to very low flows, slowing
summertime water renewalin the Salish Sea. South Sound had unusually low oxygen.
2016 Year in Review: Aerial photography
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EOPS Weather Climate Species Respond Water column Aerial photos
11. Strait of
Juan de Fuca
San Juan Islands
Padilla Bay
Main Basin
Hood Canal
South Sound
Whidbey Basin
11
10
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Aerial photography
& navigation guide
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Willapa Bay
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EOPS Weather Climate Species Respond Water column Aerial photos
12. Brown-colored water of Duck Lake stained by humus (soil/organic material)flowing intocoastal bays.
Location: Ocean Shores (Grays Harbor), 10:46 AM.
Plume
suspendedsediments
suspendedsediment
Large number of seals hauled out on a
sand bank in the middle of the bay.
Aerial photography 2-8-20161 Navigate
EOPS Weather Climate Species Respond Water column Aerial photos
13. Incoming tide at the entrance to Grays Harbor. Colors indicate three different water masses.
Location: Westhaven State Park(Westport),10:48 AM.
Aerial photography 2-8-2016
2
1
3
2 Navigate
EOPS Weather Climate Species Respond Water column Aerial photos
14. Aerial photography 3-16-2016
Jellyfishpatches in green water, colored by a spring bloom.
Location: Budd Inlet (South Sound),3:16 PM.
cloud reflection
jellyfish
jellyfish
jellyfish
3 Navigate
EOPS Weather Climate Species Respond Water column Aerial photos
15. Aerial photography 3-16-2016
Suspended fine sediments lining all beaches around Discovery Park.
Location: Seattle (Central Sound),2:42 PM.
sediment
sediment
4 Navigate
EOPS Weather Climate Species Respond Water column Aerial photos
16. Water rich in phytoplankton from Peale Passage flowing past Boston Harbor.
Location: Off Dover Point, near Dana Passage (South Sound),12:33 PM.
boat
boat
Bloom
Debris
Debris
5 NavigateAerial photography 4-6-2016
EOPS Weather Climate Species Respond Water column Aerial photos
17. A.
A. Schooling fish or eelgrass,keeping them apart remains a guessing game! B. Internal waves in bay.
Location:A. Battle Point,B. Manzanita Bay,Bainbridge Island(CentralSound),1:01 PM.
eelgrass
B.
fish?
Debris
internal waves
6 NavigateAerial photography 4-6-2016
EOPS Weather Climate Species Respond Water column Aerial photos
18. A. B.
A. Organic material washing onto beaches and decaying. B. Very strong spring bloom conditions.
Location: West side of Budd Inlet (South Sound),4:44 PM.
Bloom
boat
marker
Public submission of picture, by Laura Uhis
7 NavigateAerial photography 5-2-2016
EOPS Weather Climate Species Respond Water column Aerial photos
19. Large and numerous accumulations of organic material at the surface. Phytoplankton bloom.
Location: Dyes Inlet (Central Sound),5:19 PM.
boat
Debris
Bloom
boat
8 NavigateAerial photography 5-2-2016
Debris
EOPS Weather Climate Species Respond Water column Aerial photos
20. Organic material accumulating in large ribbons along tidal front at the entrance to Budd Inlet.
Location: Across from Boston Harbor,Budd Inlet (South Sound),12:51 PM.
boat
Debris
Debris
Debris
9 NavigateAerial photography 6-27-2016
EOPS Weather Climate Species Respond Water column Aerial photos
21. Large patches of jellyfish,sediment-richriver plume,and red-brown bloom near easternshore.
Location: Totten Inlet (South Sound),12:59 PM.
Bloom
jellyfish
boat
boat
jellyfish
jellyfish
mussel rafts
Plume
10 NavigateAerial photography 6-27-2016
EOPS Weather Climate Species Respond Water column Aerial photos
22. Red-brown bloom and large patches of jellyfish. Turquoise water is likely freshwater.
Location: Across from YoungCove,Eld Inlet (South Sound),3:08 PM.
boat
Bloom
jellyfish
jellyfish
jellyfish
jellyfish jellyfish
jellyfish
jellyfish
boat
jellyfish
turquoise
11 NavigateAerial photography 7-20-2016
EOPS Weather Climate Species Respond Water column Aerial photos
23. Very large mats of organic material drifting in Port Madison and adjacent parts of Central Basin.
Location: Point Monroe,Bainbridge Island(CentralSound),3:58 PM.
12 NavigateAerial photography 7-20-2016
EOPS Weather Climate Species Respond Water column Aerial photos
24. Strong red-brown bloom, abundant jellyfishpatches and organic debris at surface.
Location: Budd Inlet (South Sound),2:25 PM.
Bloom
boat
jellyfish
logs
Debris
Debris
Debris
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
Bloom
Debris
13 NavigateAerial photography 8-24-2016
EOPS Weather Climate Species Respond Water column Aerial photos
25. Strong red-brown bloom and abundant jellyfishpatches.
Location: Eld Inlet (South Sound),2:28 PM.
boat
Bloom
boat
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
14 NavigateAerial photography 8-24-2016
EOPS Weather Climate Species Respond Water column Aerial photos
26. Large accumulations of a Noctiluca bloom at an unusual time of the year.
Location: Entrance to Pickering Passage,Case Inlet (South Sound),2:48 PM.
boat
Debris
Debris
Bloom
boat
Debris
Pickering Passage
15 NavigateAerial photography 8-24-2016
EOPS Weather Climate Species Respond Water column Aerial photos
27. Strong red-brown bloom, jellyfishpatches, and organic debris at surface.
Location: Near Big Tykel Cove, Budd Inlet (South Sound),12:28 PM.
boat
Bloom
Bloom
jellyfish jellyfish
Debris
boat
boat
boat
16 NavigateAerial photography 9-26-2016
EOPS Weather Climate Species Respond Water column Aerial photos
28. Large tidal eddy and water with different colored blooms.
Location: LibertyBay (Central Sound), 1:01 PM.
Bloom
Bloomv
Bloom
eddy
17 NavigateAerial photography 9-26-2016
EOPS Weather Climate Species Respond Water column Aerial photos
29. Red-brown bloom and flood tide settingoff eddy. River plume with suspended sediment on easternshore.
Location: Port Gamble (Hood Canal),1:06 PM.
barge
barge
Bloom
eddy
mussel raft
Plume
boat
18 NavigateAerial photography 9-26-2016
EOPS Weather Climate Species Respond Water column Aerial photos
30. ship
Abundant jellyfishpatches.
Location: Budd Inlet (South Sound),12:18 PM.
jellyfish
jellyfish
jellyfish jellyfish
jellyfish
jellyfish
jellyfish
19 NavigateAerial photography 11-22-2016
EOPS Weather Climate Species Respond Water column Aerial photos
31. Large quantities of suspended sediment and eddies off easternshores of Steamboat Island.
Location: SquaxinPassage (South Sound),12:31 PM.
eddy
sediment
sediment
eddy
eddy
eddy
Steamboat Island
20 NavigateAerial photography 11-22-2016
EOPS Weather Climate Species Respond Water column Aerial photos
32. Marine Waters Program Marine Sediment Program BeachProgram
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EOPS Weather Climate Species Respond Water column Aerial photos