Greg Mattingly, MD, founding partner of St. Charles Psychiatric Associates in St. Louis, Missouri and Associate Clinical Professor of Psychiatry, Washington University.

Interview courtesy:   Supernus Pharmaceuticals
Website for more information:   Qelbree.com

Attention-Deficit/Hyperactivity Disorder (ADHD) is one of the most common psychiatric diagnoses in adults that affects ~1 in 16 adults and 1 in 10 children in the U.S. The condition is defined as a persistent pattern of inattention and/or hyperactivity-impulsivity that can interfere with daily life.

ADHD symptoms can include inattention (like struggling to pay attention or stay organized), hyperactivity (like being restless or talking excessively) and impulsivity (like interrupting or acting without thinking). However, ADHD symptoms aren’t always universal, especially when it comes to men and women. These symptoms can have a serious impact on those living with it and can lead to people having a hard time performing daily activities or fulfilling work responsibilities because of symptoms.

Despite ADHD being a 24/7 chronic disorder, there are options for those living with the condition to help manage symptoms, which can include a combination of behavioral management techniques as well as medication. When it comes to treatment options, there is no one-size-fits-all, and sometimes it takes trying several treatment options to figure out which works. For people with ADHD, the first step is in recognizing symptoms and having open and honest conversations with a trusted healthcare provider.

To shed light on ADHD during the awareness month, Dr. Mattingly is available for interviews to discuss how ADHD can present, various treatment options, and relevant data for doctor-patient conversations. He can also speak to:

What ADHD is and how it is known to affect the brain

How men and women may experience ADHD differently, plus symptoms that are often overlooked

Ways for managing symptoms, whether for the individual or their family and loved ones

The evolving ADHD treatment landscape and updated information on how one non-stimulant treatment option interacts with the body

The post ADHD Awareness Month in October Living with the Condition & What to Know About Evolving Treatments, NOT ONLY FOR YOUNG PEOPLE! appeared first on Good News!.

Listen to “Dominican Day Parade August 2025” on Spreaker.

The National Dominican Day Parade in New York City is a parade organized by people of Dominican heritage in the city. The event started in 1982 as a local celebration with concerts and cultural events in the Washington Heights section of Manhattan. Organized by Dominican American community leaders, the parade is held annually in August on 6th Avenue.

Similar parades to celebrate the culture of the Dominican Republic are also held every year in Haverstraw, New York, Paterson, New Jersey, Boston, Lawrence, Massachusetts, Philadelphia, Providence, Rhode Island, and along the Grand Concourse in The Bronx.

#DominicanDayParade #DDP2025

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Global Warming Acceleration: Impact on Sea Ice

02 April 2025
James Hansen, Joe Kelly, Pushker Kharecha

Abstract. Global warming has accelerated.[2] Warming melts sea ice, but it also melts ice sheets, ice shelves, ice caps and glaciers, which affects sea ice cover. Injection of cold freshwater and icebergs into the ocean tends to increase sea ice cover during a transient period until the climate forcing stabilizes and a new climate state is approached. Sea ice melt due to the warming ocean has the upper hand over freshwater injection in both hemispheres today, and thus global sea ice cover is near a historic low (Fig. 1). Arctic sea ice has been relatively stable for the past 10-20 years while Antarctic sea ice has declined, but global warming acceleration may alter both cases. In the Arctic, warm Atlantic water is intruding under the cold Arctic surface layer and warm Pacific water is spilling over the Aleutian sill into the Arctic Basin. Paleoclimate data show that warming at depth can lead to sudden loss of sea ice near Greenland, with consequences for the Greenland ice sheet. In the Antarctic, accelerated ocean warming increases melting of ice shelves and freshwater injection, which can cause temporary growth of sea ice cover. Global climate models employed by the Intergovernmental Panel on Climate Change (IPCC) have failed to account well for the freshwater effect on sea ice cover, thus contributing to IPCC’s underestimate of climate sensitivity. Overall, accelerated global warming does not bode well for stability of the ice sheets, the ocean’s overturning circulations, and global sea level in coming decades – despite the complexity of sea ice changes and uncertainty about the growth rate of ice sheet mass loss.

Global sea ice cover is one of the three big “fast” climate feedbacks in the classical definition of equilibrium climate sensitivity (ECS), which the Charney report[3] cemented. The Charney committee’s decision to exclude the “slow” feedbacks of ice sheets and the carbon cycle in their assessment was invaluable, as it allowed focus on the crucial water vapor, cloud and ice/snow feedbacks, and their interactions, in the global climate models (GCMs) then under development. Charney realized that the excluded feedbacks may have effects on short timescales, but those could be kept in mind for later study.

Recently, we concluded that climate sensitivity is high, ECS = 4.5 ± 0.5°C (1σ) for doubled atmospheric CO₂, based on three independent analyses (glacial-interglacial climate change, 1850-2024 global warming, and Earth’s darkening during 2000-2024).[2] High ECS changes everything: it fundamentally alters expectations for continued climate change. Why? Because “fast” feedbacks are not really fast: they come into play in proportion to temperature change, not in direct response to climate forcing. Thus, climate response time is approximately proportional to climate sensitivity squared.[4] One consequence is that the “fast” feedback response to ship aerosol reduction[2] is still growing significantly after five years, which is the reason we expect 2025 global temperature to be about as high as in 2024, despite the El Nino having faded to the ENSO-neutral state. A second result is that we must simultaneously consider “fast” and “slow” feedback effects because their timescales overlap. Let’s start with sea ice.

Fig. 2. Arctic and Antarctic sea ice area (31-day running-mean of daily data) from National Snow and Ice Data Center daily sea ice extent data.[1] The most recent 15 days (shown be a dotted line) are 29-day, 27-day… 3-day, 1-day means, and are thus estimates that will be replaced as data are updated.

Sea ice cover is now near its minimum during the era of global satellite data (i.e., since 1979) in both hemispheres (Figs. 2 and 3). The warm-season minimum of Arctic sea ice decreased sharply in 2007 and even further in 2012. The 2007 decrease was associated with sustained wind anomalies that drove ice from the Arctic toward warmer water and the Fram Strait.[6],[7] The 2012 melt was enhanced by an intense cyclonic storm that mixed heat upward in a normally well-stratified summer ocean, thus melting sea ice from below.[8] As the thickness of sea ice declines, such weather anomalies melt ice more effectively.

Fig. 3. Arctic and Antarctic sea ice area, with the solid curves being the 365-day running-mean of National Snow and Ice Data Center daily sea ice extent data[1] and the squares being annual results.

Sea ice volume is an important diagnostic because reduction of ice volume is a freshwater injection onto the ocean that can affect ocean circulation. Sea ice volume change is more difficult to measure than area change. Remarkably, changes of the ice “freeboard” (the height of the ice surface above sea level) can be detected by satellite, but measurement accuracy is limited, especially for Antarctic sea ice, which is less thick than Arctic sea ice. Sea ice volume estimates for the entire ocean (Fig. 4) are based on ice-ocean data assimilation models constrained by available observations. The difference between results from two data assimilation models for Arctic sea (Fig. 4, left) is one measure of uncertainty in sea ice volume changes. [PIOMAS (Pan-Arctic Ice-Ocean Modeling and Assimilation System) and GIOMAS (Global Ice-Ocean Modeling and Assimilation System) employ different ocean and sea ice models.[10]] The PIOMAS data set is preferred for the Arctic because it has been more extensively validated and used.[11]

Fig. 4. Sea ice volume: solid curves are 12-month running-mean of PIOMAS and 365-day running-mean of GIOMAS data, both from the Polar Science Center of the University of Washington.[5]

The volume of Arctic sea ice declined of the order of 10,000 cubic kilometers in the 40 years 1980-2020, thus about 250 km³/year, a freshwater injection rate comparable to the annual mass loss rate of the Greenland ice sheet. This decrease of Arctic sea ice volume over the past several decades provides a substantial term to the total freshwater injection that affects stability of the Atlantic Overturning Meridional Circulation (AMOC), as discussed in the Supplementary Material of our recent paper.[2] Total freshwater injection from all sources is now large enough to affect ocean temperature, salinity, and overturning ocean circulations, as shown, for example, in observed zonal-mean ocean temperature change (Fig. 5A)[12] and in our climate simulations.[13] However, increase of freshwater injection is absent or underestimated in models employed by the Intergovernmental Panel on Climate Change (IPCC), as shown by the absence of cooling in their climate model simulations (Fig. 5B,C) and underestimates of the freshening of polar surface waters.

Fig. 5. (A) Observed zonal-mean 2001-2020 ocean temperature relative to 1981-2000, (B) ensemble mean of CMIP6 for that period, and (C) CMIP6 result for 2081-2100 (from Fig. 1, Shu et al., 2022).[10]

Climate sensitivity. Failure of IPCC models to capture the cooling from freshwater injection affects IPCC’s best estimate for equilibrium climate sensitivity (ECS) because IPCC relies heavily on comparison of climate simulations for 1850-present with observed global warming. Models that fail to capture the freshwater effect – which causes a delay of polar warming and reduced global warming – require unrealistically low ECS in order to avoid global warming that exceeds observations. However, this effect on estimated ECS is exceeded by the aerosol effect described next.

Aerosols are the main reason for IPCC’s underestimate of climate sensitivity. IPCC’s estimate of aerosol climate forcing (Fig. 3 of ref. 2) is nearly linear in global sulfur emissions (Fig. SM1 of ref. 2). With the IPCC aerosol forcing, an ECS of about 3°C for doubled CO₂ is required to yield close agreement with observed global warming over the past century. However, the impact of aerosols on clouds (which is most of the aerosol forcing) is highly nonlinear; we conclude in paper 2 that global aerosol forcing increased (became more negative) by about 0.5 W/m² during the period 1970-2005 as a result of human-made aerosols being spread more globally into more pristine air, including over the ocean. Aerosols thus reduced the net human-made (greenhouse gas plus aerosols) climate forcing, and as a result a higher climate sensitivity (4.5°C ± 0.5°C for doubled CO₂) is required to match observed global warming. This high climate sensitivity is also best able to simulate the strong warming in the past two years, and it is the main reason that we expect little if any cooling in the annual mean 2025 global temperature.

Two additional – independent and consistent – evaluations of climate sensitivity are provided by (1) comparison of paleoclimate equilibrium states,[14] and (2) inference of large amplifying cloud feedback based on accurate monitoring of Earth’s radiation balance.[2]

Summary implications. High climate sensitivity (including the implied corollary that human-made aerosols have partly offset greenhouse gas warming) changes everything. Most important: it makes it much more difficult to avoid passing the “point-of-no-return” – shutdown of the Atlantic Meridional Overturning Circulation (AMOC) and, in turn, sea level rise of several meters.

AMOC shutdown occurs when the density of the upper ocean in the regions of deepwater formation in the North Atlantic becomes sufficiently light relative to deeper ocean layers, i.e., light enough to prevent the winter sinking of surface water that drives the global ocean conveyor. Accelerated warming has three effects that increase the likelihood of AMOC shutdown and the speed with which shutdown can occur: (1) accelerated global warming limits mixing of the warmed surface water with deeper, colder, layers, (2) greater warming increases precipitation, adding freshwater to the surface layer; and (3) greater warming increases ice melt and thus increases freshwater injection onto the North Atlantic.

AMOC shutdown is the “point-of-no-return” because it requires centuries for the ocean circulation to recover from shutdown and, in the meantime, transport of heat from the Southern Hemisphere into the North Atlantic is greatly reduced. Resulting increase of ocean temperature in the Southern Hemisphere practically locks in demise of the West Antarctic ice sheet, with sea level rise of several meters.

Evaluation of how close the world is to AMOC shutdown is extremely difficult. IPCC’s approach – relying almost entirely on global climate models – is fraught with uncertainty and errors, as suggested by a paper[15] concluding that AMOC would not shut down even with 5°C global warming and by the IPCC AR6[16] conclusion that AMOC shutdown is low probability.

More reliable analysis, we argue, requires comparable emphasis on information obtained from (1) paleoclimate, (2) global climate models, and (3) ongoing observations of climate change and climate processes. That is the approach that we will follow at Climate Science, Awareness and Solutions (CSAS) and we appreciate support that allows us to continue to pursue that research. We plan to make available and continually update a broad array of the most essential data, e.g., the sea ice graphs are here.[17] However, timely results in support of policy needs are dependent on continuation and enhancement of crucial observations. We draw attention especially to:

(1) the global ARGO float program[18] of several thousand deep-diving autonomous floats, which needs to be continued and expanded with more capable floats in the polar regions that can assess changes near vulnerable ice shelves and in the sub-sea-ice ocean. The United States National Oceanic and Atmospheric Administration (NOAA) has provided a large fraction of these floats, but it is unclear whether they can be counted on to continue and to enhance the observations. It is important for more nations to step up their contributions to the program.

(2) the global Earth radiation budget measurements presently obtained by CERES[19] instruments nearing their end-of-life. It is not clear that NASA has adequate plans for continuation of the measurements. In any case, it would be very useful if the European Union and/or China carried out measurements with a quality comparable to the high-precision NASA data and made the data freely available.

[1] Sea ice extent is defined by NSIDC (National Snow and Ice Data Center) as the ocean area with sea ice concentration exceeding 15%. NSIDC Artic Sea Ice News and Analysis and daily updates of sea ice extent for the Arctic and Antarctic are available from NSIDC.
[2] JE Hansen, P Kharecha, M Sato et al., Global warming has accelerated: are the United Nations and the public well-informed? Environment: Science and Policy for Sustainable Development, 67(1), 6–44, 2025, https://doi.org/10.1080/00139157.2025.2434494
[3] J Charney et al., Carbon Dioxide and Climate: A Scientific Assessment. (Washington: National Academy of Sciences Press, 1979)
[4] J Hansen, G Russell, A Lacis et al. Climate response times: dependence on climate sensitivity and ocean mixing. Science 229, 857-9, 1985
[5] Polar Science Center. Data. Applied Physics Laboratory, University of Washington. (last accessed 31 March 2025), https://psc.apl.uw.edu/data/
[6] J Zhang, RW Lindsay, A Schweiger, I. Rigor, What drove the dramatic retreat of Arctic sea ice during summer 2007?, Geophys Res Lett, 35, doi:10.1029/2008GL034005
[7] RW Lindsay, J Zhang, A. Schweiger et al, Arctic sea ice retreat in 2007 following thinning trend, J Clim 22, 165-76, 2009
[8] J Zhang, R Lindsay, A. Schweiger, M Steele, The impact of an intense cyclone on 2012 Arctic sea ice retreat, Geophys Res Lett 40, 720-6, 2013
[9] J Zhang, DA Rothrock, Modeling global sea ice with a thickness and enthalpy distribution model in generalized curvilinear coordinates, Mon. Wea. Rev., 131(5), 681-97, 2003
[10] S Liao, H Luo, J Wang et al., An evaluation of Antarctic sea-ice thickness from the Global Ice-Ocean Modeling and Assimilation System based on in situ and satellite observations, The Cryosphere, 16, 1807-19, 2022
[11] J Zhang, private communication, 27 March 2025
[12] Q Shu, Q Wang, M Arthum et al., “Arctic Ocean amplification in a warming climate in CMIP6 models,” Sci. Adv. 8, eabn9755, 2022
[13] J Hansen, M Sato, P Hearty et al., “Ice melt, sea level rise and superstorms: evidence from paleoclimate data, climate modeling, and modern observations that 2 C global warming is highly dangerous,” Atmos Chem Phys 16, 3761-812, 2015. See also the Supplementary Material of reference 2
[14] JE Hansen, M Sato, L Simons et al., “Global warming in the pipeline,” Oxford Open Clim. Chan. 3 (1) (2023): doi.org/10.1093/oxfclm/kgad008
[15] P Bakker, A Schmittner, JTM Lenaerts et al., Fate of the Atlantic Meridional Overturning Circulation: strong decline under continued warming and Greenland melting. Geophy Res Lett; 43, 12252-60, 2016
[16] IPCC. Climate Change 2021: The Physical Science Basis [Masson-Delmotte V, Zhai P, Pirani A et al. (eds)]. Cambridge and New York: Cambridge University Press, 2021
[17] Various data sets are being revised and updated, to be made available at https://www.columbia.edu/~jeh1/Data
[18] K. von Schuckmann, L Cheng, ND Palmer et al., “Heat stored in the Earth system: where does the energy go?” Earth System Science Data 12, 2013-41, 2020
[19] NG Loeb, GC Johnson, TJ Thorsen et al., “Satellite and ocean data reveal marked increase in Earth’s heating rate,” Geophys Res Lett 48, 2021: e2021GL093047

https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=5e918e2921&e=ac34793166

Donate to CSAS Columbia

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On October 1st, the CTA Foundation hosted an Accessibility Roundtable at Verizon’s Technology and Policy Center in Washington, D.C., to mark the start of Disability Employment Month.

The event featured insights from Assistant Secretary Taryn Williams and a panel of CTA Foundation and Mitsubishi Electric America Foundation grant recipients, discussing the future of accessibility in technology.

Thanks to our sponsors—Verizon, Mitsubishi Electric America Foundation, and Brunswick Corporation—and to everyone who attended and contributed to the conversation.

3. Save the date for #GivingTuesday on December 3rd

The CTA Foundation Health Innovation Challenge, thanks to a seed grant from the WITH Foundation, asks consumer technology companies to leverage their products to solve challenges faced by those with intellectual or developmental disabilities (IDD) in accessing digital health care.

The post CTA Foundation News: Meet the 2025 CES Eureka Park® Accessibility Contest Winners appeared first on Good News!.

Featuring the personalities and cultural significance of

Bessie Smith, Billie Holiday, Dinah Washington, Dorthy Dandridge, Lena Horne,

Josephine Baker, Mahalia Jackson, and Eartha Kitt

This tremendous theater piece offers audiences the opportunity to peer into the lives of eight women who gave unselfishly to the world some of the greatest soul-stirring music, regardless of their personal lives. These “Legendary Divas” spent their lives pleasing audiences through their music, while deep inside they were going through hell trying to fit in and be accepted as women with dreams, ambitions, needs, wants and desires.

It is imaginatively packaged in the modern day story of a beautiful 21year old young black woman (Michelle Harris) and her 23 year old Jewish boyfriend Joshua Greene. The year is 2024. Michelle is a talented artist and a graduate of New York University. Josh is in his last year of New York University Law School and is being interviewed by major New York law firms.

They met at a college social gathering. It was “love at first sight”. They are deeply devoted to each other’s lives and involved with their respective careers. Josh is on the road to success as an “A” student in both undergraduate school and law school. Michelle is a very bright young college graduate having great difficulty getting her theatrical career off the ground. She has a callback to audition for one of the great famous black singers in a show.

Joshua wishes he could help but he can’t….until he comes up with an interesting idea.

THE INTERNET!!!

He suggests that she go online and research these famous singers. Look at their videos…listen to their music. It will be a great experience for her. Michelle loves the idea.

As she begins her Internet journey the artists appears. They have discussions with each other about the trials and tribulations, they had to go through, to be recognized with the great gifts God had given them in the world of show business. The show is set to original music written by “Mickey” Stevenson.

The Musical travels back in time to meet these famous black superstars focusing on their trials, tribulations and determination …and yet it all happens in real time as the audience watches.

To enhance the story, projections take us to Paris, London, Hollywood and New York City. The Michelle character actually sends us to Detroit and adds the sounds of Motown music, too.

HERE IS A SONG THAT MICKEY CO-WROTE FOR THE GEORGE FLOYD TRADEDY. it is a very powerful song words, arrangement, visuals and performer who brought it together as though you were the one who couldn’t breathe

https://youtu.be/qf6LPgf1h-A?si=uD-HPk2O4NIVZd16

Mickey Stevenson is a member of the Song Writers Hall of Fame and was the first A&R Executive at Motown. He was intimately involved not only with the development of Martha Reeves and the Vandellas career, but also influential in discovering and developing the careers of The Four Tops, The Supremes, Marvin Gaye, Stevie Wonder, and The Temptations.

Mickey also started Motown’s in-house band famously known as the “Funk Brothers,” and was always on the look-out for young writers who he brought to Motown including Ron Milner (originally a pizza salesman in Chicago) who went on to write the mega-hit, “For Once In My Life” — which both Stevie Wonder and Tony Bennet made famous.

Mickey Stevenson’s own “Dancing in the Streets” remains a pop classic that not only Martha and the Vandellas recorded but so did The Mamma & the Papas, David Bowie and Mick Jagger, Little Richard, The Grateful Dead and The Carpenters.

Without a doubt, Mickey Stevenson’s talent and pioneering impact on the music industry will be felt in spaces and places for many years to come

#mickeystevenson #singitfromtheheart #motown #a&rman #music #soulmusic #BessieSmith #BillieHoliday #DinahWashington #DorthyDandridge #LenaHorne #JosephineBaker #MahaliaJackson #EarthaKitt #motownmusic

The post MOTOWN’S FIRST A&R MAN, MICKEY STEVENSON’S BOOK & HIS SING IT FROM THE HEART A New Musical By Mickey appeared first on Good News!.

The post Creation Nation, Arts and Peace, Horizon Plaza, 9/27/23 4pm appeared first on Good News!.

KATYA GRINEVA, CELEBRATED CARNEGIE HALL PIANIST

Field Arts & Events Hall is honored to host renowned pianist Katya Grineva for a benefit concert on July 16th at 3PM.

The program, titled “Love & Water,” will include a selection of romantic classics chosen by Ms. Grineva to celebrate Field Hall’s waterfront location and the beauty of the Olympic Peninsula. This unique program will be performed only once as a special gift from Ms. Grineva to honor the opening of the brand new Donna M. Morris Theater inside Field Hall and help us close our Capital Campaign.

The benefit concert will also recognize the extraordinary support from Founders Circle Patrons and Donors, including Dorothy Field, the donor and arts patron for whom the building has been named. The celebration will conclude with a champagne toast inside the new conference center overlooking the Strait of Juan de Fuca.

Known as a pianist of exceptional romantic and poetic expression, Ms. Grineva holds the distinction of having been invited to perform at Carnegie Hall more than any other solo female pianist in the organization’s history. Her performance style has been described as “liquid… dreamlike” by the New York Times.

Tickets for this special event are available to Founders Circle donors who have contributed any amount in support of the Capital Campaign. We thank you for your support!

Original link: https://fieldhallevents.org/katya/

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National Engineers Week gets underway on February 19th – which coincides with the birthday of President George Washington – America’s first engineer. It is also a time to emphasize the importance of learning math, science, and technical skills. Observances like this help ensure a diverse workforce by increasing understand of and interest in engineering careers.

Engineers play a crucial role in the growth and welfare of the nation by solving the toughest engineering challenges. With sustainability as a guiding principle, engineers work to strengthen the nation’s security by building and maintaining America’s water resources infrastructure and providing military facilities where service members train, work and live.

Learn more about engineering roles – especially in the Army Reserve– during this important segment.

National Engineers Weekcalls attention to the significant contributions of engineers at our nation’stop organizations, including the U.S. Army Reserve.Engineers play a vital role in the growth and welfare of the nation by solvingthe toughest challenges. With sustainability as a guiding principle, ArmyReserve engineers work to strengthen the nation’s resilience by building andmaintaining infrastructure and water resources.

With roots dating backto the American Revolution in 1778, the Army continues to prioritizeengineering and innovation at home and abroad. The U.S. Army Corps of Engineersis researching and developing technology for our Soldiers stationed in othercountries. These Soldiers are also using their expertise to protect and restoreAmerica’s environment including critical efforts in the Everglades, theLouisiana coast, and along many of our nation’s major waterways. Army ReserveSoldiers have the advantage of bringing unique civilian skills such as smallbusiness management and advanced engineering degrees to the job, making themparticularly well-suited for emergency and disaster response.

Engineering roles arecritical positions within all military branches, especially the Army Reserve.Observances like National Engineers Week help ensure a diverse workforce byraising awareness and understanding of and generating interest in engineeringcareers.

Good News is shared by Army Reserve ColonelAndrew Sinelli, Commander, 301st Forward Engineer Support Team-Main, to learn more about the vital role engineers fulfill in theArmy Reserve. Col. Sinelli will discuss the latest achievements and high-demandSTEM capabilities found in the Army Reserve. Interview courtesy: U.S. ArmyReserve

The post A Week Dedicated to Engineers: They Create Devices Solving Our Most Complex Problems appeared first on Good News!.

Nurse who sang all the time in her hospital is given the honor to sing for President Biden & the world at the Washington Memorial in honor of the 400,000 who died 1/19/21 Thanks ABC News

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