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_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
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
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_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
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_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_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. 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.
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
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
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_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
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_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_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. 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.
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.
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_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_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_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
Dr. Christopher Krembs, with the marine monitoring unit of the Department of Ecology, presented on the warm water conditions in Puget Sound. He discussed the impacts on marine food webs and potential scenarios in 2015. He presented at the June 2015 NRC meeting.
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.
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.
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!
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!
Lower than expected air temperatures and sunshine are now both increasing; rivers are generally running high. Willapa Bay unfolds its beauty from a bird’s-eye view. The spring phytoplankton bloom is picking up in Puget Sound. A large red-orange-brown bloom persists in southern Hood Canal at a scale sufficient for the MODIS satellite to pick up. Jellyfish are still going strong in southern inlets. Ocean climate indices (PDO, NPGO and Upwelling Index) explain much of the variability in Puget Sound temperature, salt and oxygen. Nutrients, however, are steadily increasing while sub-surface algal pigments (chlorophyll a) are declining!
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_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
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!
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
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.
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 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.
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.
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
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.
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.
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_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_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_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
Dr. Christopher Krembs, with the marine monitoring unit of the Department of Ecology, presented on the warm water conditions in Puget Sound. He discussed the impacts on marine food webs and potential scenarios in 2015. He presented at the June 2015 NRC meeting.
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.
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.
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!
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!
Lower than expected air temperatures and sunshine are now both increasing; rivers are generally running high. Willapa Bay unfolds its beauty from a bird’s-eye view. The spring phytoplankton bloom is picking up in Puget Sound. A large red-orange-brown bloom persists in southern Hood Canal at a scale sufficient for the MODIS satellite to pick up. Jellyfish are still going strong in southern inlets. Ocean climate indices (PDO, NPGO and Upwelling Index) explain much of the variability in Puget Sound temperature, salt and oxygen. Nutrients, however, are steadily increasing while sub-surface algal pigments (chlorophyll a) are declining!
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_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
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!
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
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.
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 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.
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.
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
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.
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.
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.
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.
Natural farming @ Dr. Siddhartha S. Jena.pptxsidjena70
A brief about organic farming/ Natural farming/ Zero budget natural farming/ Subash Palekar Natural farming which keeps us and environment safe and healthy. Next gen Agricultural practices of chemical free farming.
"Understanding the Carbon Cycle: Processes, Human Impacts, and Strategies for...MMariSelvam4
The carbon cycle is a critical component of Earth's environmental system, governing the movement and transformation of carbon through various reservoirs, including the atmosphere, oceans, soil, and living organisms. This complex cycle involves several key processes such as photosynthesis, respiration, decomposition, and carbon sequestration, each contributing to the regulation of carbon levels on the planet.
Human activities, particularly fossil fuel combustion and deforestation, have significantly altered the natural carbon cycle, leading to increased atmospheric carbon dioxide concentrations and driving climate change. Understanding the intricacies of the carbon cycle is essential for assessing the impacts of these changes and developing effective mitigation strategies.
By studying the carbon cycle, scientists can identify carbon sources and sinks, measure carbon fluxes, and predict future trends. This knowledge is crucial for crafting policies aimed at reducing carbon emissions, enhancing carbon storage, and promoting sustainable practices. The carbon cycle's interplay with climate systems, ecosystems, and human activities underscores its importance in maintaining a stable and healthy planet.
In-depth exploration of the carbon cycle reveals the delicate balance required to sustain life and the urgent need to address anthropogenic influences. Through research, education, and policy, we can work towards restoring equilibrium in the carbon cycle and ensuring a sustainable future for generations to come.
WRI’s brand new “Food Service Playbook for Promoting Sustainable Food Choices” gives food service operators the very latest strategies for creating dining environments that empower consumers to choose sustainable, plant-rich dishes. This research builds off our first guide for food service, now with industry experience and insights from nearly 350 academic trials.
Willie Nelson Net Worth: A Journey Through Music, Movies, and Business Venturesgreendigital
Willie Nelson is a name that resonates within the world of music and entertainment. Known for his unique voice, and masterful guitar skills. and an extraordinary career spanning several decades. Nelson has become a legend in the country music scene. But, his influence extends far beyond the realm of music. with ventures in acting, writing, activism, and business. This comprehensive article delves into Willie Nelson net worth. exploring the various facets of his career that have contributed to his large fortune.
Follow us on: Pinterest
Introduction
Willie Nelson net worth is a testament to his enduring influence and success in many fields. Born on April 29, 1933, in Abbott, Texas. Nelson's journey from a humble beginning to becoming one of the most iconic figures in American music is nothing short of inspirational. His net worth, which estimated to be around $25 million as of 2024. reflects a career that is as diverse as it is prolific.
Early Life and Musical Beginnings
Humble Origins
Willie Hugh Nelson was born during the Great Depression. a time of significant economic hardship in the United States. Raised by his grandparents. Nelson found solace and inspiration in music from an early age. His grandmother taught him to play the guitar. setting the stage for what would become an illustrious career.
First Steps in Music
Nelson's initial foray into the music industry was fraught with challenges. He moved to Nashville, Tennessee, to pursue his dreams, but success did not come . Working as a songwriter, Nelson penned hits for other artists. which helped him gain a foothold in the competitive music scene. His songwriting skills contributed to his early earnings. laying the foundation for his net worth.
Rise to Stardom
Breakthrough Albums
The 1970s marked a turning point in Willie Nelson's career. His albums "Shotgun Willie" (1973), "Red Headed Stranger" (1975). and "Stardust" (1978) received critical acclaim and commercial success. These albums not only solidified his position in the country music genre. but also introduced his music to a broader audience. The success of these albums played a crucial role in boosting Willie Nelson net worth.
Iconic Songs
Willie Nelson net worth is also attributed to his extensive catalog of hit songs. Tracks like "Blue Eyes Crying in the Rain," "On the Road Again," and "Always on My Mind" have become timeless classics. These songs have not only earned Nelson large royalties but have also ensured his continued relevance in the music industry.
Acting and Film Career
Hollywood Ventures
In addition to his music career, Willie Nelson has also made a mark in Hollywood. His distinctive personality and on-screen presence have landed him roles in several films and television shows. Notable appearances include roles in "The Electric Horseman" (1979), "Honeysuckle Rose" (1980), and "Barbarosa" (1982). These acting gigs have added a significant amount to Willie Nelson net worth.
Television Appearances
Nelson's char
Characterization and the Kinetics of drying at the drying oven and with micro...Open Access Research Paper
The objective of this work is to contribute to valorization de Nephelium lappaceum by the characterization of kinetics of drying of seeds of Nephelium lappaceum. The seeds were dehydrated until a constant mass respectively in a drying oven and a microwawe oven. The temperatures and the powers of drying are respectively: 50, 60 and 70°C and 140, 280 and 420 W. The results show that the curves of drying of seeds of Nephelium lappaceum do not present a phase of constant kinetics. The coefficients of diffusion vary between 2.09.10-8 to 2.98. 10-8m-2/s in the interval of 50°C at 70°C and between 4.83×10-07 at 9.04×10-07 m-8/s for the powers going of 140 W with 420 W the relation between Arrhenius and a value of energy of activation of 16.49 kJ. mol-1 expressed the effect of the temperature on effective diffusivity.
Artificial Reefs by Kuddle Life Foundation - May 2024punit537210
Situated in Pondicherry, India, Kuddle Life Foundation is a charitable, non-profit and non-governmental organization (NGO) dedicated to improving the living standards of coastal communities and simultaneously placing a strong emphasis on the protection of marine ecosystems.
One of the key areas we work in is Artificial Reefs. This presentation captures our journey so far and our learnings. We hope you get as excited about marine conservation and artificial reefs as we are.
Please visit our website: https://kuddlelife.org
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and write to us if you have any questions:
info@kuddlelife.org
1. Surface Conditions Report, September 26, 2016
Eyes Over Puget Sound
Field log Climate Water column Aerial photos Continuous monitoring Streams
Publication No. 16-03-077
Up-to-date observations of water quality conditions in Puget Sound and coastal bays
Start here
Scuba info
Critter of the Month– The Sweet Potato Sea Cucumber
2. Dr. Christopher
Krembs (Editor)
Personalimpressions p. 4
September is jellyfish season!
Climateinfluences p. 6
Sunny, warm,and dry conditions withlow river flows.
Watercolumn p. 7
Lower oxygenwasobservedinsouthernPuget Sound in August.
Water in coastal bays was saltier due to lack of rain.
Aerialphotography p. 11
Large jellyfishaggregations inSouth Sound. Red-brownand
green-brownblooms were widespreadinmany bays across
Puget Sound andthe San JuanIslands. Incontrast,Central Sound
had clear water withlittle algal activity.
Continuous monitoring p. 35
Algal concentrations are decreasingacross Central Basinwith
some short-termgrowthinmid-September.
Streams p. 37
InAugust, many streams had slipped back to below-normal
flows. Precipitationevents inSeptember improvedPuget Sound
streamflows.
LONG-TERMMARINEMONITORINGUNIT
Skip Albertson
Julia Bos
Suzan Pool
Editorial assistanceprovided by: Suzan Pool, CarolMaloy
Marine conditionsfrom 9-26-2016at a glance
Field log Climate Water column Aerial photos Continuous monitoring Streams
Jim
Shedd
JuliaSuzan
Mattie Michalek
3. Critter of the Month – The Sweet Potato Sea Cucumber
Personal Field Impression
Field log Weather Water column Aerial photos Continuous monitoring Streams
Eyes Under Puget Sound 9-26-2016
Field log Climate Water column Aerial photos Continuous monitoring Streams
Learn more about Molpadiaand othercritters on Ecology’s EcoConnect blog here.
Angela Eagleston& Dany Burgess
Marine Sediment Monitoring Team
Fun Facts!
• Their skeleton is composed of
tiny particles called ossicles.
• They eat upside down with
their faces buried in the mud.
• They are smooth and shiny
because they lack tube feet.
Molpadiaintermedia
This critter sounds like a vegetable
and looks a bit like a breakfast
sausage, butthe structures in its skin
make it special! Find out what
makes this plump mud-dweller an
important partof Puget Sound
benthic communities.
4. Personal Field Impression
Field log Weather Water column Aerial photos Continuous monitoring Streams
Personal Field Impression 9-26-2016
Field log Climate Water column Aerial photos Continuous monitoring Streams
Our WCC intern, Mattie Michalek, presented a projecton the large jellyfish
masses wehave been seeing in Budd Inlet. Mattie analyzed photos frommonthly
EOPS flights over the last 6 years. Sheassigned jellyfish images to 5 categories to
indicate how abundantthe jellyfish mass aggregations (smacks) were.
Mattie presented her study
results at the 2016 South Sound
Science Symposium: “Do
salinity and temperaturein
Budd Inlet drivejellyfish mass
aggregations?”
September is jellyfish season in South Sound!
Jellyfish biomass reached
record levels in Budd Inlet
and other finger inlets of
South PugetSound in the
fall of 2014 and summer of
2015, coinciding with ‘the
Blob’ of unusually warm
water and with the drought.
Budd Inlet 2014
View poster
5. This isa newfeatureandwearesolicitingfeedback (salb461@ecy.wa.gov).
Eventuallywewill featurethemostrecentdata.
good poor
visibility
Find depths with high and low visibility
• Best visibility wasabout35 feet or more
around SeacrestPark in Elliott Bay.
• Poor visibility occurred in many places of
Puget Sound within the first10 feet of the
surface.
• In August, visibility took a downturn
perhaps in responseto abundantsunshine
and resultantplanktonic blooms.
• Elliott Bay decreased visibility from42 ft to
36 ft since July.
• We usetransmissometer readings fromour
CTD packageand convertthem into
horizontalvisibility.
What was the visibility in the water for divers?
Personal Field ImpressionThe divers' page, visibility 9-26-2016
Field log Weather Water column Aerial photos Continuous monitoring StreamsField log Climate Water column Aerial photos Continuous monitoring Streams
August
6. Climate Influences leading to 9-26-2016
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.
August Summary:
Air temperatures wereslightly
abovenormal.
Precipitationwas below
normal.
Sunshine levels werehigher.
River flows werestill below
normal, particularly to the
north (Nisqually River is
regulated).
Upwelling, ENSO, and PDO are
abovenormal.
higher No datalowerexpected
*UpwellingAnomalies (PFEL)
PDO = PacificDecadal Oscillation
NPGO = North Pacific GyreOscillation
ENSO = El Niño Southern Oscillation
Field log Weather Water column Aerial photos Continuous monitoring StreamsField log Climate Water column Aerial photos Continuous monitoring Streams
7. We usea boatand
a chartered float plane
equipped with a CTD
package
to access our monthly
monitoring stations.
We communicate data
and environmental
marine conditions using:
1. Marine Water
Condition Index
(MWCI)
2. Eyes OverPuget
Sound (EOPS)
3. Anomaliesand
sourcedata
Field log Climate Water column Aerial photos Continuous monitoring Streams
Ourlong-termmarinemonitoringstationsinWashington
Starthere
Isl.
.
Station network of abmient
water quality monitoring stations
8. Field log Climate Water column Aerial photos Continuous monitoring Streams
HowwellisPugetSoundexchangingitswater?
Year 2016 continues to have record-breakingglobal temperatures. Inour region,the Fraser River flow has plummeted.
Estuarine circulationis important because water temperatures inPuget Sound are still warmer thannormal! The Fraser
River is the largest freshwater source for the SalishSea,significantly affectinganddriving estuarine circulation.
Inwinter andspring 2016, the Fraser
River and other rivers dischargedprematurely. This
year’s Fraser River summer flow has been extremely
low in response to warmwinter temperatures and
lack of snowpack inBC. Very low summer flows
inhibit the renewal of water inPuget Sound. The
flow is now normalizing.
Source: http://wateroffice.ec.gc.ca/index_e.html
Very low Fraser River flow this
summer meant stagnant
water inthe Salish Sea and
reducedexchange with
coastal water.
As a consequence,water
warmedandpollution hada
chance to accumulate.
Credit: Christopher Krembs
0
2000
4000
6000
8000
10000
12000
Dec-13
Jan-14
Feb-14
Mar-14
Apr-14
May-14
Jun-14
Jul-14
Aug-14
Sep-14
Oct-14
Nov-14
Dec-14
Jan-15
Feb-15
Mar-15
Apr-15
May-15
Jun-15
Jul-15
Aug-15
Sep-15
Oct-15
Nov-15
Dec-15
Jan-16
Feb-16
Mar-16
Apr-16
May-16
Jun-16
Jul-16
Aug-16
Sep-16
Discharge(m3s-1)
Higher than normal
Lower than normal
Expected
Fraser RiverFlow
9. Physical conditionstracked in historicalcontext
Explore profiles
at all stations
Temperature Normalizing Oxygen lowerSalinity higher
Region
7 8 9 10 11 12 1 2 3 4 5 6 7 8 9 10 11 12 1 2 3 4 5 6 7 8 7 8 9 10 11 12 1 2 3 4 5 6 7 8 9 10 11 12 1 2 3 4 5 6 7 8 7 8 9 10 11 12 1 2 3 4 5 6 7 8 9 10 11 12 1 2 3 4 5 6 7 8
Whidbey Basin
Hood Canal
Central Sound
South Sound
Grays Harbor
Willapa Bay
North Sound
San Juan
2015 2015 201620152016 2016
After nearly 2 years of record-breakingwater temperatures,Puget Soundtemperatures andsalinity are not
quite to expectedranges inAugust. Lower oxygenconditions continue insouthernPuget Sound. At the
coast,salinity is higher due to very low river flows (see page 37).
Field log Climate Water column Aerial photos Continuous monitoring Streams
10. a) PacificDecadalOscillationIndex(PDO,temperature) (explanation)
b) UpwellingIndex(anomalies)(Upwelling,low oxygen) (explanation)
c) NorthPacificGyreOscillationIndex(NPGO, productivity) (explanation)
Field log Climate 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 long-term variability: (a)water is still warm (PDO), (b) upwellingoflow
oxygen and high nutrient ocean water are normal (UpwellingIndex anomaly),and (c) surface productivity
alongthe coast is normalizing(NPGO).
-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
11. Summary: Aerial photography9-26-2016
Large jellyfishaggregations were infinger Inlets of SouthSound. Red-brownandgreen-brownblooms
were widespreadin many bays across Puget Soundand aroundthe San JuanIslands. Incontrast,
Central Soundhad clear water withlower algal activity.
Field log Climate Water column Aerial photos Continuous monitoring Streams
Start here
Mixing and Fronts:
Many and large tidal eddies outlined by blooms of different
colors.
Debris:
Largeorganic debris rafts in Budd and Case Inlets and
Nisqually Reach.
Visible blooms:
Strong red-brown blooms in South Sound and in Sinclair,
Liberty, and Samish Bays. Brown-green blooms seen around
tidal eddies. In Totten, Eld, and Dyes Inlets.
Jellyfish:
Very numerous in Budd, Eld, and Totten Inlets. Not seen in
other inlets.
BloomDebrisFront Suspendedsediment:
Near shoresuspended sediments mostly due to strong tidal
activity. Some regional river input of suspended sediment.
Plume
Blooms in Budd Inletwithstrikingintensity
SinclairInletwith red-brownbloom
Bloom
Bloom
jellyfish jellyfish
12. Strait of
Juan de Fuca
San Juan Islands
Padilla Bay
Main Basin
Hood Canal
South Sound
Whidbey Basin
Field log Climate Water column Aerial photos Continuous monitoring Streams
Sunny, very good visibility
Flight Information:
Aerial photography
and navigation guide
Flight route
9
3
2
8
Tide data(Seattle):
Time Height (ft) High/Low
01:29 AM 9.13 H
08:02 AM 0.75 L
03:29 PM 10.94 H
09:27 PM 4.55 L
6
11
14
41
Observation Maps:
Central and NorthSound
South Sound
15
12
13
7
5
18
19
20
16
10
17
13. Strong red-brown bloom, jellyfishpatches, and organic debris at surface.
Location: Near Big Tykle Cove,Budd Inlet (South Sound),12:28 PM.
1 Aerial photography 9-26-2016 Navigate
Field log Climate Water column Aerial photos Continuous monitoring Streams
boat
Bloom
Bloom
jellyfish jellyfish
Debris
boat
boat
boat
14. Two differently colored red-brown blooms and abundant jellyfishpatches.
Location: Across Butler Cove, Budd Inlet (South Sound),12:31 PM.
Bloom
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
jellyfish
2 NavigateAerial photography 9-26-2016
Field log Climate Water column Aerial photos Continuous monitoring Streams
jellyfish
jellyfish
boat
marker
jellyfish
Bloom
boat
boat
jellyfish
jellyfish
16. A. B.
4 Navigate
Field log Climate Water column Aerial photos Continuous monitoring Streams
Aerial photography 9-26-2016
A. Red-brown and green blooms around tidal eddy during incoming tide. B. Large patch of organic debris.
Location: A. Eld Inlet,B. Budd Inlet (South Sound),12:37 PM.
Bloom
boat
Debris
Bloom
Debris
boat
Debris
eddy
17. A.
5 NavigateAerial photography 9-26-2016
Field log Climate Water column Aerial photos Continuous monitoring Streams
Tidal currents and eddies with different colored blooms (green and red-brown) during incoming tide.
Location: A. Carlyon Beach,Totten Inlet,B. Hope Island (South Sound),12:39 PM.
Bloom
Bloom
B. Bloom
eddy
eddyBloom
18. Strong red-brown bloom and abundant jellyfishpatches.
Location: Henderson Bayand BurleyLagoon, Carr Inlet (South Sound),12:49 PM.
6 NavigateAerial photography 9-26-2016
Field log Climate Water column Aerial photos Continuous monitoring Streams
Bloom
suspendedsediment
Debris
mussel raft
boat
powerline
Burley
Lagoon
19. Tidal currents and eddies with different colored blooms (green and red-brown) during incoming tide.
Location: Dyes Inlet (Central Sound),12:57 PM.
7 NavigateAerial photography 9-26-2016
Field log Climate Water column Aerial photos Continuous monitoring Streams
Bloom
boat
Bloom
Debris
eddy
boat
20. Red-brown bloom in shallow embayment near Keyport.
Location: Keyport,entrance to Liberty Bay (Central Sound),1:00 PM.
8 NavigateAerial photography 9-26-2016
Field log Climate Water column Aerial photos Continuous monitoring Streams
boat
Debris
Bloom
21. Large tidal eddy and water with different colored blooms.
Location: LibertyBay (Central Sound), 1:01 PM.
9 NavigateAerial photography 9-26-2016
Field log Climate Water column Aerial photos Continuous monitoring Streams
Bloom
Bloomv
Bloom
eddy
22. 10 NavigateAerial photography 9-26-2016
Red-brown bloom with adjacent river plume.
Location: LibertyBay (Central Sound),1:02 PM.
Field log Climate Water column Aerial photos Continuous monitoring Streams
boat
Plume
Bloom
Bloom
23. NavigateAerial photography 9-26-2016
Red-brown bloom and flood tide settingoff eddy. River plume with suspended sediment on easternshore.
Location: Port Gamble (Hood Canal),1:06 PM.
Field log Climate Water column Aerial photos Continuous monitoring Streams
11
barge
barge
Bloom
eddy
mussel raft
Plume
boat
24. B.A.
NavigateAerial photography 9-26-2016
A. Red-brown bloom and suspended sediment next to Samish Island. B. Ship slowed by tug reveals that
bloom is only at surface. Location: Samish Bay(North Sound),1:31 PM.
Field log Climate Water column Aerial photos Continuous monitoring Streams
12
suspendedsediment
tug
ship
Bloom
suspendedsediment
Bloom
clear
suspendedsediment
Bloom
SamishIsland
25. NavigateAerial photography 9-26-2016
Jet from Samish Bay flowing north alongside Lummi Island. Fraser River plume/bloom and front.
Location: Lummi Island,Rosario Strait (North Sound),1:36 PM.
Field log Climate Water column Aerial photos Continuous monitoring Streams
13
Plume
Lummi Island
26. NavigateAerial photography 9-26-2016
Fraser River plume/bloom meetingflood tide which causes turbulent mixing.
Location: Rosario Strait (North Sound),1:39 PM.
Field log Climate Water column Aerial photos Continuous monitoring Streams
14
Plume
Cypress Island
27. NavigateAerial photography 9-26-2016
Fraser River plume/bloom mixing into eddy in Lopez Sound.
Location: Mud Bay,Lopez Sound (North Sound),1:47 PM.
Field log Climate Water column Aerial photos Continuous monitoring Streams
15
eddy
Plume
28. NavigateAerial photography 9-26-2016
Red-brown bloom and suspended sediment.
Location: Mud Bay,Lopez Sound (North Sound),1:47 PM.
Field log Climate Water column Aerial photos Continuous monitoring Streams
16
boat
Bloom
suspendedsediment
29. B.
A.
NavigateAerial photography 9-26-2016
Strong red-brown fillingDiscovery Bay and extendingto the bay entrance.
Location: A. West Side, B. East Side Discovery Bay (North Sound), 2:01 PM.
Field log Climate Water column Aerial photos Continuous monitoring Streams
17
Bloom
Bloom
boat
Bloom
Beckett Point
Diamond Point
30. Field log Climate Water column Aerial photos Continuous monitoring Streams
NavigateAerial photography 9-26-2016
Greenand red-brown blooms show how patchy blooms can be.
Location: Quartermaster Harbor (Central Sound), 2:30 PM.
18
boat
Bloom
boat
Bloom
Bloom
suspendedsediment
31. B.A.
NavigateAerial photography 9-26-2016
Green-brown bloom leaving Carr Inlet in a meandering ribbon betweenMcNeil and Fox Islands.
Location: Carr Inlet (South Sound),2:39 PM.
Field log Climate Water column Aerial photos Continuous monitoring Streams
19
Bloom
Bloom
Fox Island
McNeil Island
32. B.A.
NavigateAerial photography 9-26-2016
A. Large organic debris patch and B. Plume/bloom trapped in Oro Bay.
Location: AndersonIsland (South Sound),2:43 PM.
Field log Climate Water column Aerial photos Continuous monitoring Streams
20
Debris
Debris
NisquallyDelta
NisquallyDelta
Plume
Debris
33. North Sound Central Sound
Numbers on map refer to picture numbers for spatial reference
Date: 9-26-2016
Qualitative aerial observer map during transit Navigate
Numbers on map refer to picture numbers for spatial reference
Field log Climate Water column Aerial photos Continuous monitoring Streams
17
18
16
15
8
9
7
10
11
12
14
13
Port Gamble
34. Date: 9-26-2016
Qualitative aerial observer map during transit
Numbers on map refer to picture numbers for spatial reference
Navigate
South Sound
Field log Climate Water column Aerial photos Continuous monitoring Streams
1 2
3
4
5
6
19
20
35. The Victoria
Clipper IV carries
sensorsin its
sea chest. The
sensorsallow us
to plot transects
of:
A. Temperature
B. Chlorophyll
C. Turbidity
Over time,
we see the
dynamics of
these variables
in surface water
betweenSeattle
and Victoria,BC.
Field log Climate Water column Aerial photos Continuous monitoring Streams
Continuousmonitoring September2016
Summary of Victoria Clipper IVferry data:
Water temperatures continue to be warm,andCentral Basinis still warmer thanthe Juan
de Fuca Strait. Algal concentrations are decreasingacross Central Basinwithsome short-
termgrowthin mid-September. Turbidity is slightly higher in the Strait than Puget Sound,
likely causedby Fraser River sediment outflow.
C.
B.A.
Not
shown,
fouling
effects
36. Field log Climate Water column Aerial photos Continuous monitoring Streams
Continuousmonitoring September2016
Figures show daily data from
sensors installed on the ferry
which measure near-surface
waters at 5-secintervals while
the Victoria Clipper IV transits
between Seattle and Victoria,
BC.
A. Sea Surface Temperature:
Water is warmer inCentral
Basinthan the Strait.
B. Chlorophyll: Concentrations
are higher in Puget Soundthan
in the Strait.
C. Turbidity: Turbidity is low on
the entire route.
A.
C.
Victoria
Olympic
Peninsula
Seattle
Victoria
Olympic
Peninsula
Seattle
Victoria
Olympic
Peninsula
Seattle
B.
37. How have streamflows fared over Summer 2016?
Field log Climate Water column Aerial photos Continuous monitoring Streams
Jim Shedd,
Ecology
C. In August, about 30 to 50% of streams
were below normal for most of the month.
In September, streamflows increased over
the second half of the month. Currently
about 75% of the state’s streamflows are
within the normal range.
In August, many streamflows werebelow-normalfromdrier and warmer conditions.
Precipitation in September improved streamflows in Puget Sound .
A. Well below normal precipitation in the
Puget Sound basin in August resulted in
declining streamflows after conditions
temporarily had improved in July.
B. Particularly low river flows occurred in the
Olympics and north Cascades in August. (See
page 9 inceasing salinity in coastal bays)
A. C.B.
39. You may subscribe or unsubscribe to the Eyes Over Puget Sound email listservby going to:
http://listserv.wa.gov/cgi-bin/wa?A0=ECOLOGY-EYES-OVER-PUGET-SOUND
Many thanks to our business partners: Clipper Navigation,SwantownMarina,andKenmore Air.
We are looking forfeedbackto improve ourproducts.
Dr. ChristopherKrembs
christopher.krembs@ecy.wa.gov
Marine Monitoring Unit
EnvironmentalAssessment Program
WA Department of Ecology
Field log Climate Water column Aerial photos Continuous monitoring Streams