Quinnipiac’s continuing commitment to uplift neighboring communities through civic engagement, partnership and scholarship has earned a prestigious 2026 Carnegie Community Engagement Classification. The national distinction has been awarded to Quinnipiac through 2032. Learn more
Headlines from QU.edu/today				February 4, 2026
MAT students to receive up to 50% off tuition by partnering with local school districts School of Communications alumni have Patriots’ Super Bowl run covered from every angle Alumnus’ compassionate care inspires Marguerite I. Boissard Memorial Scholarship Fund at the School of Nursing Computer science students and professor present ransomware research at Las Vegas conference Off-campus students help neighbors shovel out after major snowstorm Join the ‘We Love Quinnipiac’ tour across the country Marinov, men’s ice hockey blanks St. Lawrence in 7-0 win Women’s basketball downs Fairfield to become the only undefeated team in conference Monroe’s double-double helps lift men’s basketball over Fairfield 61% of voters think the Trump administration has not given an honest account of the fatal shooting of Alex Pretti, Quinnipiac national poll finds
Stories and more at QU.edu/today
ICYMI: Four Bobcats Earn Spots at the Olympics

https://www.ne16.com/t/10233792/173971236/8820831/0/1006986/?x=904913bc

Quinnipiac will be well represented on the ice at the 2026 Winter Olympics. First-year forward Jade Barbirati ’29 will represent Team France, and Kati Tabin ’20 and Devon Toews ’17 will represent Team Canada. Women’s ice hockey assistant coach Brent Hill has also been named to the U.S. Olympic Women’s Ice Hockey staff. Learn more
Top Highlights From the Coming Week
Here are just a few of the many things happening throughout the next week at Quinnipiac: Thursday, February 5 at 8:40 a.m.: Winter Olympics Watch Party at OISS Thursday, February 5 at 12:30 p.m.: Strategic Visioning Session (Mount Carmel Campus) Thursday, February 5 at 12:30 p.m.: QU in NYC Information Session Thursday, February 5 at 12:45 p.m.: How to Get Your Start Working in the Music Industry Thursday, February 5 at 2:30 p.m.: Strategic Visioning Session (North Haven Campus) Thursday, February 5 at 7 p.m.: Men’s Basketball versus Canisius Thursday, February 5 at 8 p.m.: New Semester, New Mindset Thursday, February 5 at 9:15 p.m.: QU in LA Information Session Friday, February 6 at 6 p.m.: Indigenous Student Union Movie Night: ‘Avatar’ Friday, February 6 at 7 p.m.: Men’s Ice Hockey versus Brown Friday, February 6 at 7:30 p.m.: Dungeons and Dragons Club DM Engagement Fair Saturday, February 7 at 12 p.m.: Best Buddies Super Bowl Party Saturday, February 7 at 2 p.m.: Men’s Basketball versus Niagara Saturday, February 7 at 7 p.m.: Men’s Ice Hockey versus Yale | Game Watch Parties Set for Across U.S. Saturday, February 7 at 9 p.m.: Throwbacks Trivia Sunday, February 8 at 6 p.m.: Super Bowl Watch Party Tuesday, February 10 at 12:30 p.m.: Unfiltered Comm-versations: Bad Bunny and the Super Bowl Tuesday, February 10 at 12:30 p.m.: The Research Policies Committee Presents: Submitting Grant Proposals & The IRB Approval Process Tuesday, February 10 at 12:30 p.m.: Room Selection Information Session Tuesday, February 10 at 12:30 p.m.: Career Resource Pop-Up Tuesday, February 10 at 2 p.m.: Working at the NY Islanders Tuesday, February 10 at 5 p.m.: QU Pitch Competition Info Session Tuesday, February 10 at 8:30 p.m.: Galentine’s Bingo Tuesday, February 10 at 9:15 p.m.: Valentine’s Day Card Making for a Local Nursing Home Wednesday, February 11 at 12 p.m.: QU in DC Semester and Seminar Programs Info Session Wednesday, February 11 at 3 p.m.: Spring Law Career Networking Fair Session Wednesday, February 11 at 5 p.m.: Dessert Charcuterie Boards Wednesday, February 11 at 6 p.m.: Virtual Transfer Information Session Wednesday, February 11 at 6:30 p.m.: Valentine’s Bingo and Card Making with Old Friends and New Wednesday, February 11 at 8:30 p.m.: Self Care Night with QU Active Wednesday, February 11 at 9 p.m.: Galentine’s Day See the full listing and get all the details at calendar.qu.edu. To learn more about Common Hour, visit QU.edu/commonhour
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“At Quinnipiac, we passionately care about our community and believe everyone should feel welcome and valued. This recognition reflects our strong alignment of mission, leadership, values and resources in support of meaningful, reciprocal community engagement — work that addresses pressing societal challenges and contributes to the public good.” — Bethany Zemba, vice president for community relations Learn more
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Have a story suggestion? We’d love to hear it. Please email Quinnipiac Today editor Jamie DeLoma at jamie.deloma@qu.edu with your idea.

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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

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Direct link to tickets–

tinyurl.com/legacies23

Details—-

Monday

November 6, 2023

To be held under the rotunda at

Columbia University’s

Low Memorial Library

West 116th Street &Broadway, Manhattan

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community www.pausetheworldforpeace.org to donate. Thanks in the name of MOTHER EARTH

Pause the World for Peace,   2023 Events for Mother Earth…

Earth & Water Day Times Square LIVE 5 Hour Broadcast Concert, April 22, 2023 11:00AM – 4PM EST. TV/Podcast

JOIN US – MOTHER EARTH IS CALLING

New York, NY – For Immediate Release.  April 11, 2023.  FOR INFORMATION:            Contact paul.sladkus@goodnewsbroadcast.com and or call 212 647 1212.

WHAT & WHERE:         Earth & Water Day, April 22, 2023 LIVE IN TIMES SQUARE at 11am – 4pm est. for a LIVE 5 Hour Broadcast, also on www.facebook.com/UNIFY our broadcaster who has 130 Million Reach for Facebook Followers and received 2 Billion Hits in 2017 for Peace Day and www.youtube.com/goodnewsbroadcast with 165,000 Views last month, also in China with Weiwei Gao 200 Million Audience and around the world.  Entertainment & More…

PRESS CONFERENCE WAS HELD ON: World Water Day, March 22 Virtual Press Conference included many of the talent and corporations that will be part of Earth Day in Times Square. The Earth & Water Day Schedule will be shared shortly.   To watch the 2 hour 49 minute Press Conference & Sizzle Reel go to:   http://pausetheworldforpeace.org/2023/04/04/world-water-day-march-22-2023/

 Why:                           MOTHER EARTH IS CALLING.  Only 1% of all our water on Earth is fresh.  Tornados, earthquakes, flooding,  sea level rising, WASH (Water, Sanitation and Hygiene) causes 1.4 Million people to die and 74 million lives shorted, 1 in 4 people/2 billion lack safe drinking water, 3.6 billion lack safe sanitation, 44 % households wastewater is not safe (UN/WHO).

Key Note Speakers:      Our broadcast talent and speakers share their up-beat, life-affirming work… in essence, The Good News is what that they are doing to help Mother Earth Heal. Virtually Peace Messengers, i.e. Ringo Starr will start the broadcast and ask for a Moment of Silence for Peace, then Dr. Jane Goodall will share her concern for our environment, other celebrities, i.e. Leonardo DiCaprio, Stevie Wonder, Shakira share messages for us to do better and we will. Also virtually, Mayor Adams Citation, NYC Pastor Monrose, Executive Director Faith Based, Keynote from NYC Chief Climate Officer and Department of Environmental Protection Commissionaire Aggarwala, Reid Stowe, Soanya & Darshan 1,152 Days at Sea WORLD RECORD, UNBLINDED Sean Callagy and Andrea Cataneo, AY Young/Battery Tour/UN Sustainable Goals “Only American” Speaker,  Deloitte/Donna Szatkowski-Zych/ Partner, Inclusion Council Leader/Sustainability

Corporations: Deloitte, Virgin Hotels/NY, YOU GOT THIS KID, Quinnipiac University (GO BOBCATS!), BLUEVIEW Biodegradable Footwear, AMJ Global/Immersive Technology, Andrea Cataneo, Playa Betty/Mexican Food/Margarita, SaraBeth Restaurants/Bakery, Montauk Manor, Hugg-A-Planet, Animodules, Peace Lights, Hong Kong Dragon Boat Festival, 5 Star Diamond Award,  Fine Quality Events,  X~Stream Broadcasting, UNIFY, Times Square Alliance, New York City Parks & Recreation.

Entertainers:  Georgia Fumanti Bocelli Arranger “Angel Watching Over Me”, Indiggo Twins, Marvin Hamlisch International Music Award recipient Sophia Angelica “Flying On”, Surgeons Dr. Zhang Mt. Sinai/NY, Dr. Kalumuna, Dr. Joseph/ Uganda, Dentist Dr. Jacobs, Family Film Awards/Ms. Ma, China TV Series/Snow & Ice, Tigers, Parrots for Peace, Wonderama, Stephen Joseph/Comedy, Majid, Chip Shelton PeaceTime,  NY Friends of Clear Water, Montauk Film Festival/Surfing 50 States, South Fork Museum of Natural History (SOFO), Friends of Clearwater, Cristina Fontanelli, Paul Sladkus/Sax,

WE.net,  Charity:Water, Guardians of the Forest/Amazon, Original Play “Earth Quakes’, Michael Ress, HealRWorld, UNIFY, Host Reverend Paul Sladkus, All Faiths & Spiritual, Chris Breslin, Cristina Fontanelli, …more to come.

WE ARE ALL IN THIS TOGETHER.

WHO:                           Good News Corporation, GNC, a nonprofit, 501 C 3, est. 2002 has been creating International Peace Day Events since 2002.  They continue to support MOTHER EARTH & PEACE, with a mission to create life affirming, thought provoking, Good News, Entertainment and Events and share them with the world. Our website is www.pausetheworldforpeace.org

Later this year: The UN International Day of Peace, September 21, 2023 in Times Square 11AM-4PM est. and around the world. GNC has be strengthening this Peace message since 2002 in Central Park and Times Square.  A 9 11 Times Square Event is being planned. Ringo Starr Virtually will request a Moment of Silence for Peace at all events, 193 Countries of the UN who agreed to support the day, which asks for a MOMENT OF SILENCE, CEASE FIRE, ACTS OF KINDNESS/PEACE.

LET’S GROW TOGETHER. GOOD NEWS MOTTO: ALL WE ARE IS WHAT WE ARE WITH EACH OTHER. ZEAL

For more information contact: 

Paul Sladkus, 212 647 1212

New York, NY, Montauk, NY

PS – SPECIAL OPPORTUNITY FOR OUR FRIENDS AND MEMBERS: Looking for a vacation rental, SHORT TERM, in Montauk, NY. Call Paul Sladkus.   https://goodnewsplanet.com/montauk-manor-rental-suite-403-paul-sladkus/

call me. Paul 917 687 1790

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Listen to “PRIDE MONTH SPECIAL – University Professor and LGBTQ Youth Safe Space Initiative Founder at Stockton University by Dr. Laurie Greene” on Spreaker.

PRIDE MONTH SPECIAL Drag Queens and Beauty Queens: Contesting Femininity in the World’s Playground.

by Laurie Greene

The Miss America pageant has been held in Atlantic City for the past hundred years, helping to promote the city as a tourist destination. But just a few streets away, the city hosts a smaller event that, in its own way, is equally vital to the local community: the Miss’d America drag pageant.

Drag Queens and Beauty Queens presents a vivid ethnography of the Miss’d America pageant and the gay neighborhood from which it emerged in the early 1990s as a moment of campy celebration in the midst of the AIDS crisis. It examines how the pageant strengthened community bonds and activism, and how it has changed now that Rupaul’s Drag Race has brought many of its practices into the cultural mainstream. Comparing the Miss’d America pageant with its glitzy cisgender big sister, anthropologist Laurie Greene discovers how the two pageants have influenced each other in unexpected ways.

Drag Queens and Beauty Queens deepens our understanding of how femininity is performed at pageants, exploring the various ways that both the Miss’d America and Miss America pageants have negotiated between embracing and critiquing traditional gender roles. Ultimately, it celebrates the rich tradition of drag performance and the community it engenders.
On your program, Laurie can answer questions like:

What are “camp sensibilities” in drag performance and gay culture?

The book explored the personalities of the pageants. Can you give us a flavor of them?

What is the importance of camp in missed America? Drag style, performance, and language.

Tell us about the queering of the miss America pageant? Did anybody work on both?

How do each of the four areas of competition differ on the page TA — swimsuit, evening gown, talent, and interview. There is an object and a subject section.

Who owns the pageants?

What is the Show Us Your Shoes Parade?

Do you see the talent on both sides sharing hard work, perseverance, and talent?

What are the different elements of pageantry and the meaning of individual expression when comparing beauty pageants and drag pageants? Does one try and fit in and one tries to be unique? One fits into boundaries and one tries to break boundaries.

You mentioned that drag is part of the gay community in AC but it has a male focus. Explain?

Talk about the conflicts you found between the gay community and the drag community.



“An unprecedented look at drag culture and its history in Atlantic City. A must-read for queens and their fans!”

— Sapphira Cristal ― Miss’d American 2020

“I have long wondered how the Miss America pageant maintains a conservative appeal while ignoring the known influence and involvement by the gay community. If you’ve ever known or loved Miss America, you need this history lesson.”

— Erin O’Flaherty ― Miss Missouri 2016, first openly lesbian Miss America contestant

“After 30 years in the drag business, I was surprised and elated to learn so much about drag/LGBTQ+ history in Atlantic City. The in-depth exploration of how Miss America and Miss’d America were connected and disconnected is fascinating.”

— Sherry Vine ― Drag Legend

“Through a highly entertaining, insightful, and informative combination of history, ethnography, and gender studies, Greene uncovers the long-standing influence that Atlantic City’s LGBTQ+ community has had on the Miss America Pageant.”

— Rusty Barrett ― author of From Drag Queens to Leathermen: Language, Gender, and Gay Male Subcultures

“The subject matter is fascinating.”

― Gay & Lesbian Review


Publisher: Rutgers University Press (December 18, 2020)

Language: English

Paperback: 248 pages

ISBN-10: 1978813864

ISBN-13: 978-1978813861

LAURIE GREENE is an associate professor of anthropology at Stockton University in New Jersey, where she has taught since 1986. She is the founder and chair of the LGBTQ Youth Safe Space Initiative at Stockton University and an advocate for the local LGBTQ community. Connect with Laurie On FaceBook!

Publisher: Rutgers University Press (December 18, 2020)

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