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_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_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_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
Effects of ocean currents on environmentANAMIKA RAJ
INTRODUCTION ABOUT OCEAN CURRENTS
TYPES OF OCEAN CIRCULATION
FACTORS THAT CAUSE & AFFECT OCEAN CURRENTS
EFFECT OF OCEAN CURRENT
RELATION OF OCEAN CURRENT WTH MARINE LIFE AND CLIMATE CHANGE
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.
This slides of class 7 Geography, chapter 3 ,Our Changing Earth part -2 ,
in this presentation describe exogenic force agents ;Water,Wind,Sea Weaves,and Glacier.
this is useful for teachers and students of Chhattisgarh board and CBSE Board for teaching and understanding .
there is good photos in example.
also available teaching video in you tube GURU's Channel.
https://www.youtube.com/channel/UCuf04TA3UGuLDtnlOkJVntA
CLIMATE CHANGE, SEA-LEVEL RISE and COASTAL GEOLOGIC HAZARDSriseagrant
CLIMATE CHANGE, SEA-LEVEL RISE
and
COASTAL GEOLOGIC HAZARDS
URI Climate Change Symposium
5 May 2011
Jon C. Boothroyd
Rhode Island State Geologist,
Research Professor Emeritus – Quaternary Geology
-------------
Rhode Island Geological Survey and Department of Geosciences
College of the Environment and Life Sciences
University of Rhode Island
jon_boothroyd@uri.edu
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
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.
Impact of climate change in atmosphere of oceanAshish sahu
How does climate change effect the ocean?
5 ways that climate change affects the ocean
Higher temperatures are bad for fish — and for us.
Polar ice is melting.
Rising sea levels represent a slow, seemingly unstoppable threat.
Warming oceans alter currents.
Climate change is affecting the chemistry of seawater.
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.
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
Effects of ocean currents on environmentANAMIKA RAJ
INTRODUCTION ABOUT OCEAN CURRENTS
TYPES OF OCEAN CIRCULATION
FACTORS THAT CAUSE & AFFECT OCEAN CURRENTS
EFFECT OF OCEAN CURRENT
RELATION OF OCEAN CURRENT WTH MARINE LIFE AND CLIMATE CHANGE
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.
This slides of class 7 Geography, chapter 3 ,Our Changing Earth part -2 ,
in this presentation describe exogenic force agents ;Water,Wind,Sea Weaves,and Glacier.
this is useful for teachers and students of Chhattisgarh board and CBSE Board for teaching and understanding .
there is good photos in example.
also available teaching video in you tube GURU's Channel.
https://www.youtube.com/channel/UCuf04TA3UGuLDtnlOkJVntA
CLIMATE CHANGE, SEA-LEVEL RISE and COASTAL GEOLOGIC HAZARDSriseagrant
CLIMATE CHANGE, SEA-LEVEL RISE
and
COASTAL GEOLOGIC HAZARDS
URI Climate Change Symposium
5 May 2011
Jon C. Boothroyd
Rhode Island State Geologist,
Research Professor Emeritus – Quaternary Geology
-------------
Rhode Island Geological Survey and Department of Geosciences
College of the Environment and Life Sciences
University of Rhode Island
jon_boothroyd@uri.edu
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
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.
Impact of climate change in atmosphere of oceanAshish sahu
How does climate change effect the ocean?
5 ways that climate change affects the ocean
Higher temperatures are bad for fish — and for us.
Polar ice is melting.
Rising sea levels represent a slow, seemingly unstoppable threat.
Warming oceans alter currents.
Climate change is affecting the chemistry of seawater.
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.
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.
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.
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.
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_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_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
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.
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_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
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
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.
The Great South Bay once produced half of all the hard shell clams eaten in this country. Now the bay is dying. Sewering, denitrification systems, a moratorium on fertilizers and pesticides can bring the bay back.
This presentation is about The Great South Bay, the decline of the shellfishing industry, and the effort to revitalize the bay through sewering and the reintroduction of oysters
Water Matters , Episode II 1-29-2016 Prof Sarah Meyland on Managing Long Isl...Save The Great South Bay
Long Island does nothing to manage its drinking water supply, even as we are poisoning it with toxic spills and wasting it through overuse, chiefly by wasting it on our lawns. We need at last to have a policy, or risk the future of our aquifer, and of Long Island itself.
Nitrogen Pollution and The Future of Long Island By Prof. Christopher GoblerSave The Great South Bay
How does excessive nitrogen loading effect the health and resiliency of Long Island’s coastal ecosystems?
Loss of critical habitats: Eelgrass, salt marshes
Low dissolved oxygen levels, hypoxia
Acidification, low pH
Macroalgal blooms: Sea lettuce, Ulva
Toxic algal blooms: Red, rust, brown tides
Loss or depletion of shellfisheries and finfisheries
The artist Susan Brown of Sayville Long Island has painted a series of 72 paintings, all double sided, for a total of 144 paintings fo The Great South Bay, Fire Island, and The South Shore, particularly around her home town.
Susan is autistic, but at 56 years old she has established quite a reputation as an outsider artist, and as a painter in residence at Pure Vision Arts in Chelsea. Her CV can be found here. http://www.purevisionarts.org/artists/susan-brown/.
East Wind Blow Out Of The Great South Bay (courtesy Michael Busch and greatso...Save The Great South Bay
What happens when the wind comes from the east on The Great South Bay? The water is pushed west. The eastern part of the bay starts to empty out, while, as you will see, the water piles up in the west.
This slide show presents what Bellport Bay, on the Eastern Great South Bay, looks like during a strong easterly wind (slides 2-10, courtesy Michael Busch) and what the results are in Lindenhurst (slides 11-12, courtesy Michael Patrick.
Water Worries -- Nitrogen From Septic Tanks, Fertilizer, Poor Sewage Treatmen...Save The Great South Bay
Prof Christopher Gobler of Stony Brook University, a global expert on algal blooms and their causes, presents his overview of Long Island's nitrogen pollution problem and how that is triggering destructive algal blooms throughout our bays. The main culprit? 500,000 septic tanks.
Two of the charter members of The Long Island Clean Water Partnership, The Citizen's Campaign For The Environment, and The Group For The East End, offer this overview of the state of Long Island's waters -- what is polluting them and what we can do about it. The CCE's Adrienne Esposito and the GFTEE by Bob DeLuca.
Long Island gets its drinking water from the ground. Whatever we do on the surface eventually makes it into the aquifer, and into our drinking water, our rivers and bays.
The largest issue is nitrates from septic tanks, from the 200+ small sewage treatment plants, and from fertilizer, both residential and commercial leaching into the ground water, and then to our bays, where they trigger massive algal blooms -- brown tide, red tide, rust tide, blue green algae. These blooms have already destroyed much of our bay's habitats, resulting in a collapse of the shellfish and finfish population. To reverse this situation, we must impose much stricter limits on how much nitrogen can enter into our ground water from the plants, farms, and from the 500,000 septic tanks that dot Long Island.
Another major threat to Long Island water is VOCS (volatile organic chemicals). While there are 254 superfund sites on Long Island, the largest source of these VOCs are household products -- cleaners, paint strippers, aerosols. 100,000 tons of household hazardous waste is disposed of improperly every year in New York.
A further threat is the 117 pesticides now found in our drinking water. Even when banned, they remain in our environment for decades.
Finally, the improper disposal of household pharmaceuticals means that these drugs are entering into our ecosystem, with effects unknown. We must stop flushing or throwing out unused prescriptions, but dispose of them only at designated county locations.
In all, there are a number of things we can do now to help LI become sustainable for future generations: Push for new technologies and new policies that would limit nitrogenous waste from our septic and sewer systems. Stop using high nitrogen lawn and agricultural fertilizers. Dispose of your household waste properly. Any chemical you use at home will end up in the ground water unless disposed of properly. Don't pour oils, grease, and chemicals down the drain. Use green, friendly home cleaning products.
Finally, since the major contributor to Long Island's water problems has been overdevelopment (without the requisite infrastructure to support it), we need to protect what green spaces we have left.
The Long Island Clean Water Coalition, formed by a group of some twenty eco-non-profits and environmental research institutions large and small have come together to to address the water quality crisis now facing Long Island. Our groundwater is polluted, and therefore our drinking water is at peril. Because our ground water is polluted, so are our lakes, streams and bays. Algal blooms wiping out habitats in our bays, shellfish beds closed because of all the nitrogenous waste now in our water.
This presentation is by Adrienne Esposito of The Citizen's Campaign for The Environment. It powerfully presents the problem we as Long Islanders face, and what we can do to bring Long Island back from the brink of disaster.
June 3, 2024 Anti-Semitism Letter Sent to MIT President Kornbluth and MIT Cor...Levi Shapiro
Letter from the Congress of the United States regarding Anti-Semitism sent June 3rd to MIT President Sally Kornbluth, MIT Corp Chair, Mark Gorenberg
Dear Dr. Kornbluth and Mr. Gorenberg,
The US House of Representatives is deeply concerned by ongoing and pervasive acts of antisemitic
harassment and intimidation at the Massachusetts Institute of Technology (MIT). Failing to act decisively to ensure a safe learning environment for all students would be a grave dereliction of your responsibilities as President of MIT and Chair of the MIT Corporation.
This Congress will not stand idly by and allow an environment hostile to Jewish students to persist. The House believes that your institution is in violation of Title VI of the Civil Rights Act, and the inability or
unwillingness to rectify this violation through action requires accountability.
Postsecondary education is a unique opportunity for students to learn and have their ideas and beliefs challenged. However, universities receiving hundreds of millions of federal funds annually have denied
students that opportunity and have been hijacked to become venues for the promotion of terrorism, antisemitic harassment and intimidation, unlawful encampments, and in some cases, assaults and riots.
The House of Representatives will not countenance the use of federal funds to indoctrinate students into hateful, antisemitic, anti-American supporters of terrorism. Investigations into campus antisemitism by the Committee on Education and the Workforce and the Committee on Ways and Means have been expanded into a Congress-wide probe across all relevant jurisdictions to address this national crisis. The undersigned Committees will conduct oversight into the use of federal funds at MIT and its learning environment under authorities granted to each Committee.
• The Committee on Education and the Workforce has been investigating your institution since December 7, 2023. The Committee has broad jurisdiction over postsecondary education, including its compliance with Title VI of the Civil Rights Act, campus safety concerns over disruptions to the learning environment, and the awarding of federal student aid under the Higher Education Act.
• The Committee on Oversight and Accountability is investigating the sources of funding and other support flowing to groups espousing pro-Hamas propaganda and engaged in antisemitic harassment and intimidation of students. The Committee on Oversight and Accountability is the principal oversight committee of the US House of Representatives and has broad authority to investigate “any matter” at “any time” under House Rule X.
• The Committee on Ways and Means has been investigating several universities since November 15, 2023, when the Committee held a hearing entitled From Ivory Towers to Dark Corners: Investigating the Nexus Between Antisemitism, Tax-Exempt Universities, and Terror Financing. The Committee followed the hearing with letters to those institutions on January 10, 202
Honest Reviews of Tim Han LMA Course Program.pptxtimhan337
Personal development courses are widely available today, with each one promising life-changing outcomes. Tim Han’s Life Mastery Achievers (LMA) Course has drawn a lot of interest. In addition to offering my frank assessment of Success Insider’s LMA Course, this piece examines the course’s effects via a variety of Tim Han LMA course reviews and Success Insider comments.
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
Francesca Gottschalk - How can education support child empowerment.pptxEduSkills OECD
Francesca Gottschalk from the OECD’s Centre for Educational Research and Innovation presents at the Ask an Expert Webinar: How can education support child empowerment?
Acetabularia Information For Class 9 .docxvaibhavrinwa19
Acetabularia acetabulum is a single-celled green alga that in its vegetative state is morphologically differentiated into a basal rhizoid and an axially elongated stalk, which bears whorls of branching hairs. The single diploid nucleus resides in the rhizoid.
Embracing GenAI - A Strategic ImperativePeter Windle
Artificial Intelligence (AI) technologies such as Generative AI, Image Generators and Large Language Models have had a dramatic impact on teaching, learning and assessment over the past 18 months. The most immediate threat AI posed was to Academic Integrity with Higher Education Institutes (HEIs) focusing their efforts on combating the use of GenAI in assessment. Guidelines were developed for staff and students, policies put in place too. Innovative educators have forged paths in the use of Generative AI for teaching, learning and assessments leading to pockets of transformation springing up across HEIs, often with little or no top-down guidance, support or direction.
This Gasta posits a strategic approach to integrating AI into HEIs to prepare staff, students and the curriculum for an evolving world and workplace. We will highlight the advantages of working with these technologies beyond the realm of teaching, learning and assessment by considering prompt engineering skills, industry impact, curriculum changes, and the need for staff upskilling. In contrast, not engaging strategically with Generative AI poses risks, including falling behind peers, missed opportunities and failing to ensure our graduates remain employable. The rapid evolution of AI technologies necessitates a proactive and strategic approach if we are to remain relevant.
Palestine last event orientationfvgnh .pptxRaedMohamed3
An EFL lesson about the current events in Palestine. It is intended to be for intermediate students who wish to increase their listening skills through a short lesson in power point.
Adversarial Attention Modeling for Multi-dimensional Emotion Regression.pdf
Bellport dec 21_2013_b
1. The Great South Bay and the New Inlet
Bellport Middle School, Dec 21, 2013
Charles Flagg, Roger Flood, Robert Wilson and Dong-Ming Yang
Pilots: Rich Giannotti, Charles Flagg, Don Richards & Vinny Petruso
Photographers: Charles Flagg, Rich Weissman, Mike Ferrigno,
Justin Flagg, Brian Wasser, Jamie Shreeve, John Vahey,
Brad Furman, Chris Gobler and Mike Busch
http://po.msrc.sunysb.edu/GSB
22. New Inlet
~400 m2
Fire Island Inlet ~ 4000 m2
Moriches Inlet
Total
~ 800 m2
~ 4800 m2
Area
New Inlet is ~ 8% of Total
23. Velocity Survey of the Inlet, November 17, 2013
Acoustic Doppler Current Profiler (ADCP)
mounted on a 14’ skiff.
1200 kHz RDI Workhorse ADCP
24. Velocity Survey of the Inlet, November 17, 2013
Boat Track
70 round trips across main transect
from slack after high water to slack after low water.
25. Velocity Survey of the Inlet, November 17, 2013
1 m/s
Maximum observed current: 2.2 m/s (4.7 kts)
Maximum ebb transport: 445 m3/s
Total ebb transport: 6.8 x 106 m3
26. GSB Area = 216 km2
New
Inlet
Bellport Bay Area = 18 km2
Tidal range at Bellport on November 17 was 0.39 m, so the area
directly affected by the transport through the inlet was
6.8 x 106 m3 /0.39 m = 17.6 km2.
This area is approximately the size of Bellport Bay and 8% of the
larger Great South Bay.
33. Wind Direction vs Bellport Water Level
Typical Nor’easter
or
Approaching Hurricane
Cold Outbreak
with Winds from
the northwest
34. We have seen Wide Spread Sea Level Fluctuations
Woods Hole
Bellport
Lindehurst
Atlantic City
Chesapeake Bay
35.
36. Summary
The outer inlet has increased in size and moved west while the cross-sectional area has
remained relatively stable for ~9 months.
37. Summary
The outer inlet has increased in size and moved west while the cross-sectional area has
remained relatively stable for ~9 months.
With the extended spit along the western edge, the inlet is continuing its rotation and
growing longer, as happens with natural inlets.
38. Summary
The outer inlet has increased in size and moved west while the cross-sectional area has
remained relatively stable for ~9 months.
With the extended spit along the western edge, the inlet is continuing its rotation and
growing longer, as happens with natural inlets.
The inlet is relatively small compared to the other inlets, < 8% of the cross-sectional
areas with < 8% of the tidal exchange.
39. Summary
The outer inlet has increased in size and moved west while the cross-sectional area has
remained relatively stable for ~9 months.
With the extended spit along the western edge, the inlet is continuing its rotation and
growing longer, as happens with natural inlets.
The inlet is relatively small compared to the other inlets, < 8% of the cross-sectional
areas with < 8% of the tidal exchange.
There has been an increased exchange of waters with the ocean in the eastern Great
South Bay, and this has clearly improved the water quality and reduced the impact of
Brown Tides.
40. Summary
The outer inlet has increased in size and moved west while the cross-sectional area has
remained relatively stable for ~9 months.
With the extended spit along the western edge, the inlet is continuing its rotation and
growing longer, as happens with natural inlets.
The inlet is relatively small compared to the other inlets, < 8% of the cross-sectional
areas with < 8% of the tidal exchange.
There has been an increased exchange of waters with the ocean in the eastern Great
South Bay, and this has clearly improved the water quality and reduced the impact of
Brown Tides.
We experienced unusually frequent storms during last winter, which caused repeated
local flooding events but these are not historically exceptional.
41. Summary
The outer inlet has increased in size and moved west while the cross-sectional area has
remained relatively stable for ~9 months.
With the extended spit along the western edge, the inlet is continuing its rotation and
growing longer, as happens with natural inlets.
The inlet is relatively small compared to the other inlets, < 8% of the cross-sectional
areas with < 8% of the tidal exchange.
There has been an increased exchange of waters with the ocean in the eastern Great
South Bay, and this has clearly improved the water quality and reduced the impact of
Brown Tides.
We experienced unusually frequent storms during last winter, which caused repeated
local flooding events but these are not historically exceptional.
Bay waters will respond to storm-forced ocean surges, with or without the inlet.