Science Mag: Record hot summer wreaks havoc — record high temps, record low ice volume

Science Now reports that NASA says this year so far is the hottest on record in the 131 years of record keeping.  Nearly 0.7 C hotter than the average from 1951 to 1980, and NOAA has found essentially the same thing using different data.  Nightime temperatures hit record highs in 37 states of the US this summer.  The National Snow and Ice Data Center in Boulder, Colorado, has found near-record ice area loss so far this year in the Arctic Ocean, and expects the area to hit a record low this year.  Ice volume is at a record low, 10,000 cubic kilometers lower than the average of the last 30 years.  Ice volume is being lost at 17% per decade.  The open sea surface absorbs much more light energy than the white ice, trapping more heat. Since coral disease outbreaks have been reported following some bleaching events, I’d suggest people keep disease in mind for monitoring as well, if a bleaching event develops in their area.  The diseases can cause a significant proportion of the total mortality.

Doug Fenner, Coral-list 9/21/10

http://news.sciencemag.org/sciencenow/2010/09/record-hot-summer-wreaks-havoc.html?etoc=&sms_ss=email

Record Hot Summer Wreaks Havoc

by Eli Kintisch on 15 September 2010, 5:10 PM |

Hot trends.  In the Arctic, the past 4 years have had the four smallest recorded extents of sea ice.   Coral has suffered in warm water temperatures near the equator in 1997 and this year, both due in part to El Niño.

Record-breaking summer temperatures and the warmest year to date in 131 years are wreaking havoc on the global environment, say climate scientists.

The National Snow and Ice Data Center (NSIDC) in Boulder, Colorado, is about to report near-record loss of sea ice this summer, and modelers say total ice volume is at a record low. Meanwhile, the National Oceanic and Atmospheric Administration (NOAA) has issued warnings about coral bleaching throughout the Caribbean, a problem exacerbated by high water temperatures in the Atlantic Ocean.

According to NASA’s Goddard Institute for Space Studies, the first 8 months of 2010 is the warmest such January-to-August period in climate records stretching back 131 years. This period was nearly 0.7˚C warmer than the average temperature from 1951 to 1980. (NOAA announced roughly the same finding today, using many of the same temperature stations but a different analysis method.) Scorching summer temperatures set records across the United States, and nighttime temperatures hit record highs in 37 U.S. states this summer, the Natural Resources Defense Council will announce in a new report tomorrow.

Science has learned that NSIDC expects this summer to yield the third lowest area of ice “extent” in the Arctic. The ice has reached its yearly minimum, which generally occurs in September.

“Extent” means the area of icy water—essentially, areas with more than 15% of the surface covered with ice. The past 4 years have yielded the four smallest extents of sea ice in the Arctic, says NSIDC.

NSIDC climatologist Julienne Stroeve told ScienceNOW that warmer-than-average ocean temperatures were a factor in this summer’s sea-ice losses, but so are circulation patterns that push sea ice toward the pole, opening up water that can be warmed by the sun. In addition, she notes, “there’s a lot less of the old ice” in the Arctic due to its recent formation and relative thinness.

Arctic experts at the University of Washington use temperature, satellite, and weather data in a computer model to estimate the total volume of ice in the area. According to their model, the total ice volume in the Arctic is now at an all-time low, nearly 10,000 cubic kilometers less than the average of the past 30 years. “We think there is a lot of thin ice up there, but there’s little data to validate [that],” says Ron Lindsay of the University of Washington, Seattle. Overall, he says, the model suggests a stunning 17% loss of ice volume per decade.

A moderate El Niño event that began last year and ended earlier this summer has contributed to rising global ocean temperatures. El Niño periods, characterized by a redistribution of heat in the Pacific Ocean, lead to warming on the western and eastern sides of the Pacific and the western Atlantic. A very vigorous 1997–98 El Niño led to record-setting temperatures over the oceans and land. Even though this year’s warming due to El Niño is smaller, trends in ocean temperature have roughly matched 1997–98 thus far due to an overall warmer system. The trend is especially clear in waters near the equator.

The biggest immediate effect of warmer ocean temperatures in the tropics has been the extraordinary death of corals, as Science laid out 3 weeks ago:

Reefs on both sides of the Thai Peninsula were hit, with up to 100% of some coral species bleached, says James True, a coral biologist at Prince of Songkla University in Hat Yai, Thailand. He expects at least 80% of the most sensitive species to die. “A few inshore reefs got so badly damaged, they probably won’t ever come back to the way they were,” he says. Among surviving corals, “disease is rampant,” True says, with two to three times the usual incidence of necrotic lesions and growth anomalies. Similar reports of “quite extensive bleaching” have come from Vietnam and through the heart of the Coral Triangle in Indonesia and the Philippines.

Experts told Al Jazeera that up to 20% of the coral off the shore of Malaysia could die this fall. A dive instructor interviewed there said he had seen neither bleached coral nor 34˚C water in 6 years of working there. The Malaysian government has closed 13 sites to divers and snorkelers to try to mitigate the damage.

Meanwhile, in the Caribbean, according to a new bulletin put out by NOAA last week:

The NOAA Coral Reef Watch (CRW) satellite coral bleaching monitoring shows sea surface temperatures continue to remain above average throughout the wider Caribbean region. Large areas of the southeastern Caribbean Sea are experiencing thermal stress capable of causing coral bleaching. The western Gulf of Mexico and the southern portion of the Bahamas have also experienced significant bleaching thermal stress. The CRW Coral Bleaching Thermal Stress Outlook … indicates that the high stress should continue to develop in the southern and southeast Caribbean until mid-October . Bleaching stress in the western Gulf of Mexico and southern Bahamas should dissipate quickly in the next couple of weeks.

A reprieve from the sweltering temperatures is coming, but it will only be temporary. Columbia University’s Richard Seager says the now-ended El Niño phase has been followed by a La Niña phase, which usually means cooler average global ocean and land temperatures. El Niño will eventually return. More importantly, as the planet’s average temperature warms, Seager says, the El Niño-La Niña cycles “cancel one another out.”

Ohio State Un: PhD Graduate Research Opportunity In Coral Bleaching & Ocean Acidification

 

Desired (but not required) qualifications:
– MSc in Marine Science, Geology, Biology, or any physical
science.  Exceptional applicants without an MSc will also be considered.
– Experience in isotope biogeochemistry, organic chemistry, or
relevant coursework
– Tropical fieldwork experience or coral aquaculture experience
– The successful candidate must be accepted into the graduate program
in the School of Earth Sciences at The Ohio State University

The position starts in September 2011 and includes four years of
support.  Please submit applications electronically by following the
instructions at http://www.earthsciences.osu.edu/students_grad.php.
Indicate that you would like to study with Dr. Grottoli in your
application.  In addition, send a complete copy of your application
materials as a single .pdf file to Dr. Andrea G. Grottoli at
grottoli.1@osu.edu (Note: File should contain copy of your research
statement, a cover letter, resume, GRE scores, the names and contact
information of three references, and a list of relevant course with
grades).  Please indicate “Graduate student application” in the
subject line.  For more information on Dr. Grottoli’s research
program, please visit http://www.earthsciences.osu.edu/~grottoli.1.
Application deadline is 5 January 2011.  OSU is an equal
opportunity/affirmative action employer.
*******************************************************
Andrea G. Grottoli, Associate Professor
Ohio State University
School of Earth Sciences
125 South Oval Mall
Columbus, OH 43210

office:  614-292-5782
lab: 614-292-7415
cell: 215-990-9736
fax: 614-292-7688
email: grottoli.1@osu.edu

Grottoli webpage: www.earthsciences.osu.edu/~grottoli.1/
Fieldwork Micro-blog: www.twitter.com/CoralResearch
Stable Isotope Biogeochemistry Laboratory (SIB Lab):
www.earthsciences.osu.edu/~grottoli.1/SIB_Lab.html
SES seminars: www.earthsciences.osu.edu/seminars.php

Office location: 329 Mendenhall Labs
*******************************************************

Special thanks to Coral-list

Institute for Tropical Ecology & Conservation: Field Course in Coral Reef Ecology in Panama

2010 WINTER COURSE ANNOUNCEMENT (December 20th- January 9th)

FIELD COURSE IN CORAL REEF ECOLOGY (Caribbean of Panama)
http://www.itec-edu.org/coral6.html

LOCATION:  The field courses will take place at the Institute for Tropical Ecology and Conservation (ITEC) Bocas del Toro Biological Station, Boca del Drago, Isla Colon, Bocas del Toro, Panama: http://www.itec-edu.org/index.html

The Bocas del Toro (“mouths of the bull”) Biological Station is located on the north end of Isla Colón in an area known as Boca del Drago (“mouth of the dragon”). Isla Colón is the northern-most of five large islands and hundreds of smaller ones that form the Bocas del Toro Archipelago. Set in Almirante Bay on the Caribbean side of western Panama, this collection of islands is sometimes referred to as the “Galapagos of Central America”. This is because, after having been isolated for 10,000 years by geologic activity, each of the islands has evolved its own unique biota. Taking its name from Christopher Columbus who sailed into this region in 1502, Isla Colón is approximately 14 km long and 7 km wide. Isla Colón is composed primarily of limestone, and has a hilly topography supporting primary and secondary tropical rain forest. This island has a 5 km beach (Bluff Beach) on its east side, mangroves on its west side, and caves in the interior. Marine habitats include extensive turtle grass beds, hard and soft coral reefs, beaches, rocky intertidals, mangrove forests and estuaries.

Isla Colón has the highest human population in the archipelago, with most individuals living in the town of Bocas del Toro located on the far side of the island from our facility. Besides being biologically diverse, the region is also culturally diverse with a mix of Latin American, Afro-Caribbean and indigenous Ngöbe. Spanish is the official language but English is spoken. Many Ngöbe speak only their native dialect. There are only two roads on the island, both originating in the town of Bocas. One road travels along the eastern margin of the island to Bluff Beach and the other cuts through the island’s interior to Boca del Drago, where our facility is located.

INSTRUCTOR: Carlos Gustavo A. Ormond, Simon Fraser University; Conservation Science Institute; Coalición por los Tiburones (Shark Coalition), email: cormond@sfu.ca; Elizabeth McGinty (TA), University of Texas at Arlington, email: mcginty@uta.edu

COURSE LENGTH AND SCHEDULE: Winter field courses are three weeks in length (December 20th- January 9th).

TUITION: $1650 USD. Tuition fee includes all room and board, local transportation and a three-day field trip to the Boquete cloud forest on Panama’s mainland.

REGISTRATION DEADLINE: November 20, 2010. Since registration is limited to 10 students, we recommend those interested to contact the Carlos in order for him to be aware of your application.

COURSE DESCRIPTION: This course is designed to promote the desire for not only discovery and advanced understanding of coral reef ecosystems from an integrated ecological perspective but also an appreciation and understanding of the Latin American and Caribbean (LAC) culture. In addition to learning coral reef ecosystem dynamics, organism identification, and experimental design, this course will also investigate human dimensions in coral reef ecosystems, both past and present. To compliment the course and for the pure enjoyment of learning a new language, students will be taught a “Spanish for Survival” at the beginning of the session.

By taking an integrated multidisciplinary approach, this course will demonstrate the importance of melding traditional approaches to understanding and investigating coral reef ecosystems with the human dimension. A large component of the course will involve field work, complimented by lectures and discussions on daily course readings. The course will require the completion of group assignments, as well as an individual research project that may be as much sociological as it is ecological in theory. Therefore, the course will not only be of interest to those of you in the natural sciences but also those of you from the social sciences.

General Topics
•        Spanish Language
•        Environmental History and Cultural Anthropology of Panama
•        Coral Reef Formation and Oceanography
•        Coral Reef Ecology
•        Sampling Methods
•        Research Design
•        Present State of Coral Reefs
•        Coral Reef Conservation issues
•        Human Rights and the Environment in Latin America
•        Global Environmental Governance

NOTE: Dive certification is not necessary to enroll in this course, but what is required is an attraction to the ocean and a comfort in being in it. All students will require snorkel equipment (mask and fins) and those with SCUBA certification are expected to bring their own BCD, regulator, and most importantly proof of certification. There is the possibility of renting dive equipment as well as receiving dive certification from the local dive shops. If this is something that interests you, please contact Carlos for more information.

COURSE CREDIT: Up to six units of credit will be granted for these courses. Credit must be arranged by the student through his/her academic advisor and university.  Contact ITEC for details.

CONTACT: Institute for Tropical Ecology and Conservation (ITEC); 1023 SW 2nd Ave., Gainesville, FL 32601; phn: 352-367-9128, fax: 352-367-0610, email:itec@itec-edu.org., or Carlos Gustavo A. Ormond cormond@sfu.ca.  Please visit us on the web at www.itec-edu.org.  ITEC is a Non-profit (501c3) organization.

* Aunque esta clase está presentada en inglés, si sos hispanoparlante y estás interesado/a en tomar esta clase sobre los arrecifes de coral por favor comunícate conmigo, Carlos Gustavo A. Ormond
_______________________________________________

Special thanks to Coral-list

New York Times: Extreme Heat Puts Coral Reefs at Risk, Forecasts Say

 http://www.nytimes.com/2010/09/21/science/earth/21coral.html?_r=1&hp

Coral bleaching, like that seen in the Flower Garden Banks off the Texas-Louisiana border, is an indicator of heat stress.    By JUSTIN GILLIS

Published: September 20, 2010

By JUSTIN GILLIS
>From Thailand to Texas, many corals are reacting to heat stress by shedding their color and going into survival mode, putting the oceans’ richest ecosystems and fisheries at risk.
September 20, 2010
Extreme Heat Puts Coral Reefs at Risk, Forecasts Say
By JUSTIN GILLIS
This year’s extreme heat is putting the world’s coral reefs under such severe stress that scientists fear widespread die-offs, endangering not only the richest ecosystems in the ocean but also associated fisheries that feed millions of people.

>From Thailand to Texas, corals are reacting to the heat stress by bleaching, or shedding their color and going into survival mode. Many have already died, and more are expected to do so in coming months. Computer forecasts of water temperature suggest that corals in the Caribbean may undergo drastic bleaching in the next few weeks.

What is unfolding this year is only the second known global bleaching of coral reefs. Scientists are holding out hope that this year will not be as bad, over all, as 1998, the hottest year in the historical record, when an estimated 16 percent of the world’s shallow-water reefs died. But in some places, including Thailand, the situation is looking worse than in 1998.

Scientists say the trouble with the reefs is linked to climate change. For years they have warned that corals, highly sensitive to excess heat, would serve as an early indicator of the ecological distress on the planet caused by the buildup of greenhouse gases.

“I am significantly depressed by the whole situation,” said Clive Wilkinson, director of the Global Coral Reef Monitoring Network, an organization in Australia that is tracking this year’s disaster.

According to the National Oceanic and Atmospheric Administration, the first eight months of 2010 matched 1998 as the hottest January to August period on record. High ocean temperatures are taxing the organisms most sensitive to them, the shallow-water corals that create some of the world’s most vibrant and colorful seascapes.

Coral reefs occupy a tiny fraction of the ocean, but they harbor perhaps a quarter of all marine species, including a profusion of fish. Often called the “rain forests of the sea,” they are the foundation not only of important fishing industries but also of tourist economies worth billions.

Drastic die-offs of coral were seen for the first time in 1983 in the eastern Pacific and the Caribbean, during a large-scale weather event known as El Niño. During an El Niño, warm waters normally confined to the western Pacific flow to the east; 2010 is also an El Niño year.

Serious regional bleaching has occurred intermittently since the 1983 disaster. It is clear that natural weather variability plays a role in overheating the reefs, but scientists say it cannot, by itself, explain what has become a recurring phenomenon.

“It is a lot easier for oceans to heat up above the corals’ thresholds for bleaching when climate change is warming the baseline temperatures,” said C. Mark Eakin, who runs a program called Coral Reef Watch for the National Oceanic and Atmospheric Administration. “If you get an event like El Niño or you just get a hot summer, it’s going to be on top of the warmest temperatures we’ve ever seen.”

Coral reefs are made up of millions of tiny animals, called polyps, that form symbiotic relationships with algae. The polyps essentially act as farmers, supplying the algae with nutrients and a place to live. The algae in turn capture sunlight and carbon dioxide to make sugars that feed the coral polyps.

The captive algae give reefs their brilliant colors. Many reef fish sport fantastical colors and patterns themselves, as though dressing to match their surroundings.

Coral bleaching occurs when high heat and bright sunshine cause the metabolism of the algae to speed out of control, and they start creating toxins. The polyps essentially recoil. “The algae are spat out,” Dr. Wilkinson said.

The corals look white afterward, as though they had been bleached. If temperatures drop, the corals’ few remaining algae can reproduce and help the polyps recover. But corals are vulnerable to disease in their denuded condition, and if the heat stress continues, the corals starve to death.

Even on dead reefs, new coral polyps will often take hold, though the overall ecology of the reef may be permanently altered. The worst-case situation is that a reef dies and never recovers.

In dozens of small island nations and in some coastal areas of Indonesia and the Philippines, people are heavily dependent on reef fish as a source of protein. The death of corals is not immediately lethal to the fish, but if the coral polyps do not recover, scientists say the reef can eventually collapse, and the associated fishery will become far less productive.

Research shows that is already happening in parts of the Caribbean, though people there are not as dependent on fishing as those living on Pacific islands.

It will be months before this year’s toll is known for sure. But scientists tracking the fate of corals say they have already seen widespread bleaching in Southeast Asia and the western Pacific, with corals in Thailand, parts of Indonesia and some smaller island nations being hit especially hard earlier this year.

Temperatures have since cooled in the western Pacific and the immediate crisis has passed there, even as it accelerates in places like the Caribbean where the waters are still warming. Serious bleaching has been seen recently in the Flower Garden Banks, a marine sanctuary off the Texas-Louisiana border.

In Thailand, “there some signs of recovery in places,” said James True, a biologist at Prince of Songkla University. But in other spots, he said, corals were hit so hard that it is not clear young polyps will be available from nearby areas to repopulate dead reefs.

“The concern we have now is that the bleaching is so widespread that potential source reefs upstream have been affected,” Dr. True said.

Even in a hot year, of course, climate varies considerably from place to place. The water temperatures in the Florida Keys are only slightly above normal this year, and the beloved reefs of that region have so far escaped serious harm.

Parts of the northern Caribbean, including the United States Virgin Islands, saw incipient bleaching this summer, but the tropical storms and hurricanes moving through the Atlantic have cooled the water there and may have saved some corals. Farther south, though, temperatures are still remarkably high, putting many Caribbean reefs at risk.

Summer is only just beginning in the Southern Hemisphere, but water temperatures off Australia are also above normal, and some scientists are worried about the single most impressive reef on earth. The best hope now, Dr. Wilkinson said, is for mild tropical storms that would help to cool Australian waters.

“If we get a poor monsoon season,” he said, “I think we’re in for a serious bleaching on the Great Barrier Reef.”