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.
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
EOPS_November_22_2016,
ENSO is in a cold phase (La Niña) and it is wetter and warmer than normal. Strong precipitation in October greatly improved Puget Sound streamflows. At the coast, we had strong downwelling. As a result, water temperatures, salinities, and oxygen in Puget Sound are returning to normal. While surface water in Puget Sound has cooled, it is still warmer than in the Straits. Surprisingly, masses of suspended sediment occurred east of Steamboat Island in Totten Inlet. We continue to see large jellyfish aggregations in finger Inlets of South Sound and slowly fading red-brown blooms.
Publication No. 16-03-078
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
EOPS_December_14_2015,
As coastal and regional conditions gradually normalize in response to a fading Blob and increased rain, the big question remains. Will the snow in the mountains stay there or come down prematurely and lower salinity in Puget Sound like last winter? Cascade snowpack is currently below normal. The El Niño at the equator is still brewing! Major rivers transport large amounts of suspended sediments and soil into Puget Sound, also seen in our ferry sensor data. Our flight team gets in the pool for safety training.
Ecology Publication No. 15-03-079
EOPS_February_8_2016,
January air temperatures and precipitation were above normal as El Nino conditions prevail. This winter our snowpack is in much better shape, though we’ve lost some snow from the stint of warm weather. More rain and higher river flows have lowered salinities in Puget Sound and coastal bays. Nonetheless, water temperatures in Puget Sound remain at record-breaking highs. Jellyfish patches are numerous in finger inlets of South Sound and signs of phytoplankton blooms are visible in coastal bays. When conditions limit flying, Ecology’s research vessel gets the job done.
Publication No. 16-03-070
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
Sun and high air temperatures warrant en route ozone measurements for model validations. A furry visitor takes a rest on the float plane. Spotlight on our pilot, Joe Leatherman. High river flows lead to striking fronts of turquoise-colored water carrying glacial flour in many northeastern regions. Satellite and aerial images show widespread phytoplankton blooms in Whidbey Basin, Hood Canal, South Puget Sound, and West Bay of Orcas Island. Numerous large debris patches in Hood Canal, Central Sound, and South Sound Inlets. After two years of colder temperatures and higher oxygen, Puget Sound waters are returning to expected or lower dissolved oxygen levels.
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_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
EOPS_November_22_2016,
ENSO is in a cold phase (La Niña) and it is wetter and warmer than normal. Strong precipitation in October greatly improved Puget Sound streamflows. At the coast, we had strong downwelling. As a result, water temperatures, salinities, and oxygen in Puget Sound are returning to normal. While surface water in Puget Sound has cooled, it is still warmer than in the Straits. Surprisingly, masses of suspended sediment occurred east of Steamboat Island in Totten Inlet. We continue to see large jellyfish aggregations in finger Inlets of South Sound and slowly fading red-brown blooms.
Publication No. 16-03-078
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
EOPS_December_14_2015,
As coastal and regional conditions gradually normalize in response to a fading Blob and increased rain, the big question remains. Will the snow in the mountains stay there or come down prematurely and lower salinity in Puget Sound like last winter? Cascade snowpack is currently below normal. The El Niño at the equator is still brewing! Major rivers transport large amounts of suspended sediments and soil into Puget Sound, also seen in our ferry sensor data. Our flight team gets in the pool for safety training.
Ecology Publication No. 15-03-079
EOPS_February_8_2016,
January air temperatures and precipitation were above normal as El Nino conditions prevail. This winter our snowpack is in much better shape, though we’ve lost some snow from the stint of warm weather. More rain and higher river flows have lowered salinities in Puget Sound and coastal bays. Nonetheless, water temperatures in Puget Sound remain at record-breaking highs. Jellyfish patches are numerous in finger inlets of South Sound and signs of phytoplankton blooms are visible in coastal bays. When conditions limit flying, Ecology’s research vessel gets the job done.
Publication No. 16-03-070
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
Sun and high air temperatures warrant en route ozone measurements for model validations. A furry visitor takes a rest on the float plane. Spotlight on our pilot, Joe Leatherman. High river flows lead to striking fronts of turquoise-colored water carrying glacial flour in many northeastern regions. Satellite and aerial images show widespread phytoplankton blooms in Whidbey Basin, Hood Canal, South Puget Sound, and West Bay of Orcas Island. Numerous large debris patches in Hood Canal, Central Sound, and South Sound Inlets. After two years of colder temperatures and higher oxygen, Puget Sound waters are returning to expected or lower dissolved oxygen levels.
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_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
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_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
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!
Air temperatures have been slightly warmer and river flows are higher. Blooms are present only in Whidbey Basin and isolated bays. The water column otherwise is relatively clear. Sediment rich water is entering from the Stillaguamish River. Debris lines were visible in Hood Canal and North Sound. Multiple reported oil sheens seen in Lake Washington Ship Canal. Generally, the year 2014 started colder and saltier throughout Puget Sound. Oxygen is lower in Whidbey Basin, Central and South Sound, but higher in Hood Canal. Upwelling favorable conditions stimulate a spring phytoplankton bloom off the Washington coast.
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_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
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.
A recent cold spell hits Puget Sound lowlands, interrupting this year’s warmer air temperatures. The warm ocean coincides with new maximum water temperatures observed throughout Puget Sound in October! Hood Canal’s higher dissolved oxygen and cold water anomalies are disappearing. November brings cold water from Whidbey Basin into Puget Sound with moderate levels of chlorophyll fluorescence. Abundant smacks of jellyfish in finger inlets of South Sound observed from our flight. Red-brown blooms remain strong in smaller bays of South Sound. Visible suspended sediments in the coastal estuaries from rain, wind, and waves. Playing in the water? Visit our BEACH program.
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.
Puget Sound conditions are normalizing after seven months of lower oxygen. Calm, dry, cool, and foggy mornings abruptly changed on October 28 to sun and strong northerly winds. Red-brown blooms and abundant jellyfish in south Puget Sound inlets appeared as we flew to the coast. Blooms were still visible near ocean beaches and inner bays. Grays Harbor had abundant surface debris with green algae in North Bay. We spotted red-brown blooms in rivers and sloughs in Willapa Bay, as well as schooling fish near sandbanks. Many patches of suspended sediment appeared in shallow water unrelated to tidal currents and remain unexplained.
River flows are above normal and air temperatures are increasing slowly. The spring phytoplankton bloom is slow to develop with visible blooms limited to smaller bays such as Sequim and Bellingham Bays. Noctiluca observed in East Sound on Orcas Island, coinciding with high numbers of jellyfish. Debris lines are mostly confined to Hood Canal. Pockets of colder water observed in Central Sound and Hood Canal, likely from the colder, saltier conditions that developed during the winter in the northern regions. Oxygen is variable yet close to expected ranges. Sizable oil sheens were sighted in Gig Harbor and Carr Inlet.
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_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
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
Record warm water temperatures and low oxygen continue in Ecology’s Puget Sound marine monitoring station network. Record low stream flows result in visibly low river discharge into Puget Sound, in particular for the Puyallup River. Abundant sun and unusually warm water temperatures fuel phytoplankton blooms in many areas. Bright orange Noctiluca blooms are surfacing in the Commencement Bay area and around Port Madison. Finger inlets of South Sound support extensive patches of jellyfish.
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.
After a dry and sunny summer extending well into October, air temperatures are cooler than normal and precipitation has increased allowing rivers to regain strength. Despite a dry summer, Puget Sound is fresher this year than the past 17 years. As of September, warmer temperatures remained in South Sound. In October, surface water in the Straits however began to cool and the influence of rivers can be seen in our ferry data. Leaves drift on the water in South Sound and smaller blooms are confined to inlets as the productive season winds down. Meet our new intern and discover if Puget Sound really has sea spiders.
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!
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
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_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
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!
Air temperatures have been slightly warmer and river flows are higher. Blooms are present only in Whidbey Basin and isolated bays. The water column otherwise is relatively clear. Sediment rich water is entering from the Stillaguamish River. Debris lines were visible in Hood Canal and North Sound. Multiple reported oil sheens seen in Lake Washington Ship Canal. Generally, the year 2014 started colder and saltier throughout Puget Sound. Oxygen is lower in Whidbey Basin, Central and South Sound, but higher in Hood Canal. Upwelling favorable conditions stimulate a spring phytoplankton bloom off the Washington coast.
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_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
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.
A recent cold spell hits Puget Sound lowlands, interrupting this year’s warmer air temperatures. The warm ocean coincides with new maximum water temperatures observed throughout Puget Sound in October! Hood Canal’s higher dissolved oxygen and cold water anomalies are disappearing. November brings cold water from Whidbey Basin into Puget Sound with moderate levels of chlorophyll fluorescence. Abundant smacks of jellyfish in finger inlets of South Sound observed from our flight. Red-brown blooms remain strong in smaller bays of South Sound. Visible suspended sediments in the coastal estuaries from rain, wind, and waves. Playing in the water? Visit our BEACH program.
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.
Puget Sound conditions are normalizing after seven months of lower oxygen. Calm, dry, cool, and foggy mornings abruptly changed on October 28 to sun and strong northerly winds. Red-brown blooms and abundant jellyfish in south Puget Sound inlets appeared as we flew to the coast. Blooms were still visible near ocean beaches and inner bays. Grays Harbor had abundant surface debris with green algae in North Bay. We spotted red-brown blooms in rivers and sloughs in Willapa Bay, as well as schooling fish near sandbanks. Many patches of suspended sediment appeared in shallow water unrelated to tidal currents and remain unexplained.
River flows are above normal and air temperatures are increasing slowly. The spring phytoplankton bloom is slow to develop with visible blooms limited to smaller bays such as Sequim and Bellingham Bays. Noctiluca observed in East Sound on Orcas Island, coinciding with high numbers of jellyfish. Debris lines are mostly confined to Hood Canal. Pockets of colder water observed in Central Sound and Hood Canal, likely from the colder, saltier conditions that developed during the winter in the northern regions. Oxygen is variable yet close to expected ranges. Sizable oil sheens were sighted in Gig Harbor and Carr Inlet.
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_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
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
Record warm water temperatures and low oxygen continue in Ecology’s Puget Sound marine monitoring station network. Record low stream flows result in visibly low river discharge into Puget Sound, in particular for the Puyallup River. Abundant sun and unusually warm water temperatures fuel phytoplankton blooms in many areas. Bright orange Noctiluca blooms are surfacing in the Commencement Bay area and around Port Madison. Finger inlets of South Sound support extensive patches of jellyfish.
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.
After a dry and sunny summer extending well into October, air temperatures are cooler than normal and precipitation has increased allowing rivers to regain strength. Despite a dry summer, Puget Sound is fresher this year than the past 17 years. As of September, warmer temperatures remained in South Sound. In October, surface water in the Straits however began to cool and the influence of rivers can be seen in our ferry data. Leaves drift on the water in South Sound and smaller blooms are confined to inlets as the productive season winds down. Meet our new intern and discover if Puget Sound really has sea spiders.
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!
Eyes Over Puget Sound (EOPS) is a news report, and is made available within two days of observation.
http://www.ecy.wa.gov/programs/eap/mar_wat/eops/
We inform on current surface conditions in Puget Sound and links several scales of observation together. The report contains condition summaries, personal flight observations, aerial photographs, en route ferry data, satellite images, and mooring data collected by the Marine Monitoring Unit at Ecology.
Ecology's Marine Monitoring Unit conducts several marine observations with a sampling frequency of minutes to 1 month. We use our routine commute flight between Kenmore Airbase and Olympia to document current marine water conditions by camera and supplement the information with satellite images and en route ferry data between Seattle WA and Victoria BC. This program is an example to optimize monitoring resources. You may subscribe or unsubscribe to the Eyes Over Puget Sound email listserv by going to this link:
http://listserv.wa.gov/cgi-bin/wa?A0=ECOLOGY-EYES-OVER-PUGET-SOUND
Data has been increasing at an exponential rate and organizations are either struggling to cope up or rushing to take advantage by analyzing it. Hadoop is an excellent open source framework, which addresses this big data problem.
I have used Hadoop within the financial sector for the last few years but could not find any resource or book that explains the usage of Hadoop for finance use cases. The best books I have ever found are again on Hadoop, Hive, or some MapReduce patterns, with examples on counting words or Twitter messages in all possible ways.
I have written this book with the objective of explaining the basic usage of Hadoop and other products to tackle big data for finance use cases. I have touched base on the majority of use cases, providing a very practical approach.
The book sold on:
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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!
Abundant sunshine gives rise to large algal mats in South Sound, Hood Canal, and Sinclair Inlet. Red-brown algal blooms dominate in Budd, Totten, and Eld Inlets and jellyfish begin to increase. Northerly winds push algal blooms from Whidbey and Central Basins past Seattle and a bloom in northern Hood Canal southward. Satellite thermal imagery shows patterns of near-surface mixing and injection of nutrients into the surface layer. Glacial-fed rivers deliver glacial flour into Commencement Bay, stratifying the water and supporting different colored phytoplankton blooms (green, brown, and red). Since the beginning of 2013, dissolved oxygen is dropping below expected values.
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.
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.
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.
Puget Sound is feeling the heat! Starting in October, temperatures are the highest on our record since 1989. Salinity and oxygen are much lower. Recent rains have rivers flowing high. Aerial views show dramatic sediment loads from rivers mixing into otherwise blue water. But don’t be fooled – by summer, snow-fed rivers are expected to run significantly below normal, with implications for Puget Sound water quality. For details, explore the special Drought Effects segment. Spring blooms are visible only in some confined bays. Jellyfish are going strong in finger inlets of South Sound. Glimpse Puget Sound’s glacial history.
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.
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.
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.
After weeks of clouds and warmer air, blue skies and cold temperatures set in. Strong tidal fronts and sediment-rich brackish plumes leave Whidbey Basin and move into Admiralty Reach. A pod of Orcas follows the edge of the plume heading north! Red-brown blooms continue in Henderson, Eld, and northern Budd Inlets. Long organic debris lines are numerous in northern Budd Inlet, Hood Canal, and in Central Sound north of Edmonds (Triple Junction). Conditions in the water column in Puget Sound continue to normalize after seven months of lower oxygen. Water is very clear for this time of the year, particularly in the north.
The year 2013 in pictures: Low oxygen conditions persisted from January into August and broke a two year anomaly of more favorable water quality conditions (lower temperature and salinity and higher dissolved oxygen). Dramatic Noctiluca blooms appeared one month earlier than normal (May), lasted for two months and coincided with lower oxygen. Large jellyfish patches persisted over the winter but then were less visible for the rest of the year. Large drifting algal mats appeared in August.
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.
After 2-years of conditions favorable for water quality, with colder temperatures and higher oxygen, Puget Sound water conditions are closer to expected again. This year phytoplankton blooms and seasonal oxygen maxima are notable, while extensive Noctiluca blooms showed up early following a period high freshwater inputs and milder weather conditions. The Fraser River sediment influence is very strong north of San Juan Islands and warm, fresh water is entering Central Puget Sound from Whidbey Basin. In the past few weeks river flows and air temperatures have been higher than normal and now are decreasing.
Normal Labour/ Stages of Labour/ Mechanism of LabourWasim Ak
Normal labor is also termed spontaneous labor, defined as the natural physiological process through which the fetus, placenta, and membranes are expelled from the uterus through the birth canal at term (37 to 42 weeks
Safalta Digital marketing institute in Noida, provide complete applications that encompass a huge range of virtual advertising and marketing additives, which includes search engine optimization, virtual communication advertising, pay-per-click on marketing, content material advertising, internet analytics, and greater. These university courses are designed for students who possess a comprehensive understanding of virtual marketing strategies and attributes.Safalta Digital Marketing Institute in Noida is a first choice for young individuals or students who are looking to start their careers in the field of digital advertising. The institute gives specialized courses designed and certification.
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2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
A review of the growth of the Israel Genealogy Research Association Database Collection for the last 12 months. Our collection is now passed the 3 million mark and still growing. See which archives have contributed the most. See the different types of records we have, and which years have had records added. You can also see what we have for the future.
How to Make a Field invisible in Odoo 17Celine George
It is possible to hide or invisible some fields in odoo. Commonly using “invisible” attribute in the field definition to invisible the fields. This slide will show how to make a field invisible in odoo 17.
Introduction to AI for Nonprofits with Tapp NetworkTechSoup
Dive into the world of AI! Experts Jon Hill and Tareq Monaur will guide you through AI's role in enhancing nonprofit websites and basic marketing strategies, making it easy to understand and apply.
Executive Directors Chat Leveraging AI for Diversity, Equity, and InclusionTechSoup
Let’s explore the intersection of technology and equity in the final session of our DEI series. Discover how AI tools, like ChatGPT, can be used to support and enhance your nonprofit's DEI initiatives. Participants will gain insights into practical AI applications and get tips for leveraging technology to advance their DEI goals.
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.
South African Journal of Science: Writing with integrity workshop (2024)
Eops 2015 7_6
1. Surface Conditions Report, July 6, 2015
MarineWater Condition Index
Start here
Up-to-date observations of visiblewater quality conditions in Puget Sound and the Strait of Juan de Fuca
Eyes Over Puget Sound
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Publication No. 15-03-075
Guest: GabrielaHannach, King County Environmental Lab
2. Personalfieldlog p.3
Experience as a WashingtonConservationCorps
Internat Ecology.
Climateconditions p.6
Unusually warmtemperatures andsunshine continue around
the region. River systems connectedto the Puget Soundare
experiencinglower thannormal summer flows.
Watercolumn p.7
Warmwater inPuget Soundbecause of “the Blob”.
Temperatures are the highest onrecordsince 1989. Oxygenis
exhibitingnew historical minima,an unusual conditiongiven
the time of year.
Aerialphotography p.11
Very large debris islands in South andCentral Sound,
Port Susan,and Padilla Bay. Numerous patches ofjellyfish
infinger inlets of SouthSound and Sinclair Inlet.
Phytoplanktonblooms inSouthSound,smaller bays of Kitsap
Peninsula,and aroundthe San JuanIslands.
Continuousmonitoring p.36
Water is warmer andsaltier than the past 5 years.
Oxygenis near normal.
Streams p. 39
The Nooksack River has the highest nitrogenyield
of all Puget Sound Rivers!
LONG-TERMMARINEMONITORINGUNIT
Mya Keyzers
Laura Hermanson
Brooke McIntyre
Skip Albertson
Dr. Christopher
Krembs
Julia Bos
Suzan Pool
Editorial assistance provided by: Julianne Ruffner, Suzan Pool, CarolMaloy
Marine conditionsfrom 7-6-2015 at a glance
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Gabriela Hannach
Markus von Prause
3. Personal Field Impression
Fieldlog Weather Water column Aerial photos Continuous monitoring Streams
Hot and Dry: Phytoplankton & Noctiluca
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Noctiluca is a large
dinoflagellate that
often causes
conspicuousblooms
in Puget Sound.
Carotenoid pigments
fromingested algae
giveNoctiluca blooms
their characteristic
brightorangecolor:
“tomato-soupred”
Noctiluca are 0.5 mm across, with
an active tentacle that helps in the
movementof food particles.
A sample of images collected with a FlowCAMshows
variouschain-forming diatoms, including severalspecies of
the common genus Chaetoceros.
Gabriela Hannach
King County
Environmental Lab
B. Noctiluca bloomsA. Diatomscontinueto bloom in PugetSound
Circles show
concentrations
ranging from5 to
1400 cells per liter
(June15-17, 2015).Noctiluca
4. Experience as a Washington Conservation Corps (WCC) Intern at Ecology
Personal Field Impression
Fieldlog Weather Water column Aerial photos Continuous monitoring Streams
Personal Field Impression
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
ForBrooke McIntyre,work in the MarineMonitoringUnit at Ecologyis dynamicand fun.
I divide my time between water and sediment monitoring, and the BEACH program. Here’s
a peek into myexperience…
I operate a CTD and collect water
samples on marine flights.
I service moorings. The sensor at
the bottom gets covered in
barnacles! Ihelp clean these off so
it can function properlyagain.
I run chlorophyll and dissolved
oxygen lab samples.
Mt.Rainier sunrise
5. Personal Field Impression
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Learn more about the WCC and current opportunities at http://www.ecy.wa.gov/wcc
I collect sediment samples in the
field. Lookat this huge polychaete
we caught in the grab!
Advice for young
scientists:
• Be curious and always ask
questions.
• Be a volunteer. Make
connections and discover
what gets you excited.
• Be engaged. Give every
task100%.
I sort samples
for benthic
invertebrates
under the
scope.
I volunteered
on a NOAA
tow-netting
cruise.We
caught a
varietyoffish
and lots of
fried egg
jellyfish like
this one!
6. Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Climateand natural influencesthrough5-31-2015
Summary from June:
(Skip is on vacation)
Air temperatures werewarmer
than normal across Western
Washington.
Precipitation wasbelow normalin
the Puget Sound region.
Sunshine hasgenerally been
abovenormal.
River flows havealldropped,
especially the Skagit and Puyallup
Rivers. Fraser River is the only
river running still (slightly) above
normal.
PDO remains in the warmphase,
and upwelling is now above
normal.
Climate and naturalinfluences,includingweather,rivers,andthe adjacent ocean,canaffect our
marine waters. Graphics are basedonprovisional data andare subject to change.
http://www.ecy.wa.gov/programs/eap/mar_wat/weather.html.
Puttingthe puzzle piecesof influencingfactorstogether…
No data
7. We use a chartered float
plane and boat to access
our monthly monitoring
stations.
We communicate data and
environmentalmarine
conditions using:
1. MarineWater
ConditionIndex
(MWCI)
2. EyesOverPuget
Sound (EOPS)
3. Anomaliesand
sourcedata
Fieldlog Weather Water column Aerial photos Continuous monitoring Streams
Ourlong-termmarinemonitoringstationsinWashington
Starthere
Isl.
.
8. Physical conditionstracked in a statistical & historical context
Fieldlog Weather Water column Aerial photos Continuous monitoring Streams
Higher Temperature! LowerOxygenExpectedSalinity
IsWillapa Bay
returning to
normal?
Black boxes
show expected
temperatures
basedon
historicaldata
Explore profiles
atall stations
Conditions are still dominatedby warm water overall,yet some places (Willapa Bay,HoodCanal surface)
show seasonally normal temperatures. Salinity has increasedto expectedlevels andoxygenshows a mix of
expectedandlower levels inPuget Sound.
9. a) PacificDecadalOscillationIndex(PDO,temperature) (explanation)
b) UpwellingIndex(anomalies)(Upwelling,lowoxygen) (explanation)
c) NorthPacificGyreOscillationIndex(NPGO,productivity) (explanation)
Fieldlog Weather Water column Aerial photos Continuous monitoring Streams
Theoceanaffectswaterquality: OceanClimateIndices
NPGO(x10)
PDO/UpwellingIndex
Three-year running average of PDO, Upwelling, and NPGO indices scores
.
Ocean boundaryconditions are in transition: (a)water is warm (PDO), (b) upwellingoflow oxygen and
high nutrient ocean water is expected (UpwellingIndex),and (c) higher surface productivityalongthe
coast (NPGO) is expected. Where are we headingnext?
-25
-20
-15
-10
-5
0
5
10
15
20
25
-1.5
-1
-0.5
0
0.5
1
1.5
1945 1950 1955 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005 2010 2015
10. Is the food web changing in Puget Sound?
Follow the experts
WebEx
Hypothesis!
Increasesin
nitrate
concentrations
couldbe caused
by a top-down
controlon
phytoplankton
biomass.
Is Noctiluca
a visible
harbingerof a
food web
change?
Hypothesis for combining a series of recent observations
affecting energy and material transfer to higher trophic levels
Arechangesin highertropic levelspart of a story of the low food web?
11. Summary: Aerial photography7-6-2015
Massive debris islands in South and Central Sound, DyesInlet, Liberty Bay, PortSusan, and
Padilla Bay. Numerous patches of jellyfish in finger inlets of South Sound and Sinclair Inlet.
Phytoplankton bloomsin South Sound, smaller baysof Kitsap Peninsula, and San Juan Islands.
Remnantsof Noctiluca bloom near Mukilteo and East Passage.
Fieldlog Weather Water column Aerial photos Continuous monitoring Streams
Start here
Mixing andFronts:
Tidal eddy off Blake Island. Tidal frontsare nicely visible by
differentcoloration of the water in response to blooms.
Debris:
Massive occurrences in South and Central Basin, Dyes Inlet,
and Padilla Bay.
Visible blooms:
Green-brown: Totten Inlet, Dyes Inlet, PortTownsend, eastern
CentralBasin, Case Inlet.
Red-brown: Eld, Budd, and Henderson Inlets; East Sound.
Green: PortSusan.
Noctiluca: Mukilteo and East Passage.
Jellyfish:
Sizablejellyfish patches present in southern inlets of South
Sound (Budd and Eld Inlets), Sinclair Inlet, and Liberty Bay.
BloomDebrisFront
Suspendedsediment:
Reduced suspended sediments fromriver plumes found in
expected locations near rivers.
Plume
Skagit River flows are noticeably low!
View of the CTD into the water fromplane
12. Straitof
Juan de Fuca
San Juan Islands
Padilla Bay
Main Basin
Hood Canal
South Sound
Whidbey Basin
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Observation Maps:
Limited visibility,due to smoke from
Canadianforest fires that increased
haziness towards the north.
Flight Information:
11
10
Aerial photography
and navigation guide
6
Centraland NorthSound
SouthSound
7
12
5
Flight route
9
18
3
2
1
4
13
14
19
16
15
20
8
Tide data (Seattle):
03:02 AM 4.65 L
08:15 AM 9.42 H
02:46 PM -0.53 L
09:42 PM 12.46 H
17
http://earthobservatory.nasa.gov/IOTD/view.php?id=86190
July6, 2015, NASA Earth Observatory
smoke
13. Large patches of algae at the surface of Capitol Lake.
Location: Olympia (South Sound),9:34 AM.
1 Aerial photography 7-6-2015 Navigate
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Debris
Debris
Debris
14. 2 NavigateAerial photography 7-6-2015
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Numerous patches of jellyfishin water containing red-brown algal bloom.
Location: Eld Inlet (South Sound),9:37 AM.
boat
Bloom
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
15. 3 NavigateAerial photography 7-6-2015
Large islands of organic material and a front with red-brown algal bloom.
Location: Dyes Inlet (Central Sound),9:59 AM.
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
boat
Bloomboat
Debris
Debris
16. 4 Navigate
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Aerial photography 7-6-2015
Large islands of organic material and patches of jellyfish.
Location: LibertyBay(Central Sound),10:03 AM.
Bloom
Debris
Debris
jellyfish
jellyfish
boat
boat
17. 5 NavigateAerial photography 7-6-2015
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Red-brown bloom separated by front from water in Admiralty Reach.
Location: Port Townsend (North Sound),10:16 AM.
Bloom
boat
18. Bloom at surface near aquaculture pens.
Location: Penn Cove (WhidbeyBasin),10:58 AM.
6 NavigateAerial photography 7-6-2015
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
boat
boat
Bloom
19. Water rich in glacial flour from Fraser River meet red-brown bloom and reveal patterns of mixing.
Location: West of Blakely Island,San Juan Islands (North Sound),11:10 AM.
7 NavigateAerial photography 7-6-2015
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
boat
Continuous
Bloom
20. Reflectionof reddish sunlight in bays due to smoke of Canadian forest fires in BC and northerly winds.
Location: Sucia Island (San Juan Islands),11:44 PM.
8 NavigateAerial photography 7-6-2015
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
boat
red
21. A. B.
Water contain Nooksack River plume adjacent to a front with a brown bloom from Georgia Basin.
Location: A.West of Lummi Island,B. Lummi Bay(North Sound), 12:34 PM.
9 NavigateAerial photography 7-6-2015
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
boat
Bloom
Debris
Bloom
Debris
22. 10 NavigateAerial photography 7-6-2015
Large islands of organic material drifting at the surface off Samish Island.
Location: Padilla Bay(North Sound),1:05 PM.
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
ship
Bloom
Debris
Debris
Debris
Debris
23. 11 NavigateAerial photography 7-6-2015
Large islands of organic material drifting at the surface off Guemes Island.
Location: Padilla Bay(North Sound),1:05 PM.
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
boat
boat
Debris
Bloom
Front
24. Tidal fronts separating sediment-richwater from water with organic debris islands at Huckleberry Island.
Location: Guemes Island,Padilla Bay(North Sound),1:06 PM.
12 Navigate
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Aerial photography 7-6-2015
boat
Debris
Debris
25. Long debris line along tidal front separating sediment-richwater from water with glacial flour.
Location: Skagit Bay (WhidbeyBasin),1:39 PM.
13 NavigateAerial photography 7-6-2015
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Debris
Debris
Front
26. Organic debris islands, green algal bloom, and sediment-richwater show complexity of surface water.
Location: OffBeach Drive, Camano Island,Port Susan (WhidbeyBasin),1:44 PM.
14 Navigate
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Aerial photography 7-6-2015
boat
Debris
Debris
Bloom
Debris
27. 15 Navigate
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Extensive accumulations of organic debris along fronts spanning across Central Sound. Brown bloom.
Location: Between Port Madison and Shilshole (Central Sound),3:03PM.
Aerial photography 7-6-2015
boat
boat
Debris
Bloom
28. 16 Navigate
Extensive accumulations of organic debris, a brown algal bloom, and a large oil sheen.
Location: Between Port Madison and Shilshole (CentralSound),3:05PM.
Aerial photography 7-6-2015
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
boat
boat
Debris
Bloom
Front
oilsheen
29. 17 Navigate
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Tidal front linedwith organic debris separating phytoplankton-rich water enteringCentral Sound.
Location: Between Fort Worden and Blake Island (Central Sound),3:09 PM.
Aerial photography 7-6-2015
boat
Debris
Bloom
Debris
30. Diffusely structured red-brown bloom in water and macro-algae on the beach.
Location: Henderson Inlet (South Sound),3:30 PM.
18 Navigate
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Aerial photography 7-6-2015
boat
Bloom
macro-algae
32. 20 Navigate
Red-brown bloom and a tidal front.
Location: Across Frye Cove CountyPark,Eld Inlet (South Sound),3:35 PM.
Aerial photography 7-6-2015
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
boat
Bloom
Debris
33. Numbers on map refer to picture numbers for spatial reference
Date: 7-6-2015
CentralSound
Aerial photography observations in Central SoundQualitative aerial observer map during transit Navigate
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
10
Numbers on map refer to picture numbers for spatial reference
NorthSound/SanJuan Islands
3
4
5
6
7
8
9
11
12
13
14
16
15
17
34. Date: 7-6-2015
Qualitative aerial observer map during transit
Numbers on map refer to picture numbers for spatial reference
Navigate
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
SouthSound
12
20
19
18
35. Legendto map annotations
Comments:
Maps are producedby observers during and
after flights. They are intendedto give an
approximate reconstructionofthe surface
conditions onscales that connect to and
overlapwithsatellite images inthe sectionthat
follows.
Debris:
Debris canbe distinguished into natural and
anthropogenic debris floatingat the surface
sensu Moore andAllen(2000). The majority of
organic debris inPuget Sound is natural and
mixedwithdiscardedman-made pieces of
plastic,wood,etc. Fromthe plane,we cannot
differentiatethe quality of debris at the surface
andtherefore,call it for reasons of practicality
just “debris”.
S.L. Moore,M. J. Allen. 2000. Distribution of
Anthropogenicand Natural Debris on the
Mainland Shelf of the Southern California Bight.
Marine Pollution Bulletin,40(1): 83–88.
Navigate
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
36. Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Continuousmonitoring 7-6-2015
These plots show the
probability of
observationsover the
pasttwo-week period.
High probability shown in
warmcolors.
Left Panels: Density is
defined by salinity and
temperature.
Right Panel: Dissolved
oxygen concentration in
relation to salinity.
At the Mukilteo mooringstation,we continue to observe warmer than normal water
temperature. Tidal cycle and lowriver flows influence gradual increase in temperature and
salinityfor the past month. Dissolved oxygen is decreasingfor summer and is near normal levels
observed in June. Temporal patterns followa seasonal trend.
Data are not available
for this time period.
Look for themnext
month.
No oxygensensor on
the shallow instrument
package.
12-16 m depth
2-6 m depth
37. Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Continuousmonitoring 7-6-2015
Our mooringstation in Mukilteo is located
in WhidbeyBasin near Everett. It is also
located at the transition between
Possession and CentralSounds at a depth
that is influenced bythe Skagit and
Snohomish River discharges,prevailing
winds,and tidal mixing.
As the largest regional contributor of
freshwater to Puget Sound,understanding
the timingand magnitude ofthe Skagit
River flow is important.
We present dailymeans for the past 31
days. Data are plotted in PacificStandard
Time. Wind data are from Paine Field in
Everett. River flowdata are from USGS.
Click on icon to view real-time
data of the moorings
38. Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Continuousmonitoring 7-6-2015
At the Mukilteo mooring,we use the near-bottom
sensor (12-16 m deep) to measure significant inter-
annual variabilityin temperature,salinity,and
dissolved oxygen.
Inter-annual variabilityis shown over a 5-year
period. All three variables showstrongseasonality.
In June, water is warmer and saltier than past
several years. Dissolved oxygen is near normal
levels.
Seasonally,variabilityofeach parameter remains
minimal from Januaryto June.
Pleasenote that data are provisional. Data are in GMT.
39. WaterQualityofthe Nooksack River
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
Nooksack River flowing into Bellingham Bay
AtBrennen, 1995-2014:
Reddottedline = water quality met
exceptions(good)
The NooksackRiveris listed for
exceedancesin waterquality criteria for
temperatureand oxygenand has a
managementplan for bacteria.
Ecology’sRiver and StreamMonitoring
Programhasbeen obtainingwater
quality informationat the confluence of
the NooksackRiver since 1971.
Annualsediment and nutrient scores are below 80 and rangebetween moderately low to poor. Suspended
sediment loading at the confluence of the Nooksack (USGS Station 12213100) ishigh, averaging 1070 kilo tons a
year since 2011.
0
20
40
60
80
100
Fecal Coliform Oxygen pH TSS Temperature Total Nitrogen Total Phosphorus Turbidity
WQIScores
AtBrennen, 1995-2014:
Reddottedline = water quality met
exceptions(good)
40. WaterQualityofthe Nooksack River
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams
NooksackRiver represents the largest
sources of freshwater nitrogen contribution
to Puget Sound. (Von Prause, 2013).
Station
TN
(all)
NO2,3
(all)
01A050 90.54 64.43
01A120 41.39 32.35
03A060 23.56 15.93
03B050 81.3 64.15
04A100 13.48 9.4
05A070 92.04 49.2
05B070 56.18 44.74
05B110 54.24 41.24
07A090 52.89 41.4
07C070 36.63 28.61
07D050 53.37 41.44
07D130 45.36 37.39
08C070 40.39 53.49
08C110 26.78 23
09A080 52.1 36.17
09A190 21.7 16.81
10A070 36.46 23.47
11A070 29.05 19.19
13A060 49.7 41.22
16A070 34.56 13.03
16C090 9.78 5.01
18B070 10.4 4.23
Averageyieldsfor
freshwater nitrogen
(kg/sq. km/month).
“All” refersto all
months.
Data are from WY
1995 through WY
2013.
Darker shading in the
table body indicates
higher relative yield.
The NooksackRiver has the highest nitrogen
yield ofall Puget Sound Rivers!
Nooksack River
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We are looking forfeedbackto improve ourproducts.
Dr. ChristopherKrembs
christopher.krembs@ecy.wa.gov
Marine Monitoring Unit
EnvironmentalAssessment Program
WA Department of Ecology
Fieldlog Climate Water column Aerial photos Continuous monitoring Streams