Ever notice how in many parts of the world, puffy, cauliflower-shaped cumulus clouds are more common in the summer? There’s a reason for this: thermal convection. In winter, the sun has less time to heat the surface and cause instability in the atmosphere. But during the summer, heat from the sun warms the land surfaces so much that pockets of hot air—scientists call them thermals—bubble upward much like steam in a pot of boiling water. As the hot air rises, the water vapor trapped within condenses into microscopic cloud droplets. If the air is humid enough, rapidly changing cumulus clouds puff up in the atmosphere, sometimes bulging to heights above 39,000 feet. Watch in the visualizations below—based on a climate model that simulated cloud formation during a Southern Hemisphere summer—how cumulus clouds pop up over the forests of Africa and South America.

NASA Visualization Explorer, January 2012

A new study led by a NASA scientist highlights 14 key air pollution control measures that, if implemented, could slow the pace of global warming, improve health and boost agricultural production.

The research, led by Drew Shindell of NASA’s Goddard Institute for Space Studies (GISS) in New York City, finds that focusing on these measures could slow mean global warming 0.9 ºF (0.5ºC) by 2050, increase global crop yields by up to 135 million metric tons per season and prevent hundreds of thousands of premature deaths each year. While all regions of the world would benefit, countries in Asia and the Middle East would see the biggest health and agricultural gains from emissions reductions.

“We’ve shown that implementing specific practical emissions reductions chosen to maximize climate benefits would also have important ‘win-win’ benefits for human health and agriculture,” said Shindell. The study was published today in the journal Science.

NASA, January 2012

An interesting new study published in Nature points out that an increase in the strength of the Arctic Oscillation between 2005 and 2008 caused winds in the region to grow more cyclonic and shift ocean currents in ways that drew more upper-surface freshwater from Russian rivers toward the Canada Basin and the Beaufort Sea. To see the shift in the animation above, look for the tightening of the wind patterns (shown in blue) over the Canada Basin that begins about 13 seconds into the video. Notice how the stream of less salty water from river runoff in Russia (shown in red) begins to loop westward toward Canada in sync with the circulation of the wind rather than continuing toward Greenland as it typically would.

What on Earth, January 2012

I recently received word that I’ve been awarded a travel grant from the Center for a Livable Future at the Johns Hopkins Bloomberg School of Public Health. Carl Taylor Grants provide funding for research or practice projects on topics relevant to the complex interrelationships among food production, diet, environment and public health.

I’ll be doing a reporting project that looks at whether the pawpaw, a delicious but little-known fruit native to the mid-Atlantic, has the potential to emerge as a more sustainable alternative to the banana and other tropical fruits on the American market. As part of the project, I’ll be creating a special pawpaw page on my website, posting interviews with pawpaw experts, and doing as much freelancing about the pawpaw as I can.  For now, here’s a brief excerpt from the grant proposal:

A little-noticed fruit tree called the pawpaw, which is native to the mid-Atlantic region and grows in 26 states across the eastern United States, has great but largely unrealized potential to offer Americans a local and sustainable alternative to bananas and other tropical fruit. The common pawpaw (asimina triloba), a small tree that grows in shady areas with well-drained soil, produces the largest indigenous edible fruit in North America. Pawpaw fruit, which looks similar to small mangos but has fleshy yellow interiors with the texture of custard, has an extremely sweet taste that is unique but has hints of banana, mango, and pineapple.

Pawpaw has a rich but largely forgotten place in the culinary history of the United States. Prior to the arrival of Europeans, many Native American tribes used to forage for wild pawpaw and made the fruit a regular part of their diets. Lewis and Clark wrote that pawpaw saved their expedition in 1810 when food supplies ran dangerously low.  And prior to the 1920s when the banana became a cheap and ubiquitous option on the American market,  Americans across wide swaths of the eastern United States used to eat wild pawpaw in the fall.  There’s even a popular children’s song about pawpaw that is still sung frequently today.

I just returned from San Francisco where I spent a week at the American Geophysical Union’s fall meeting. With more than 21,000 attendees and tens of thousands of posters and talks, there’s never a shortage of things to see, just a shortage of time to see it all. I did a bit of blogging for What on Earth  this year. Links below:

How Satellites Can Fill the Gaps in Air Quality Maps
Airborne Particles a Threat to Himalayan Glaciers
Dust Storm Triggered Phytoplankton Blooms in the South China Sea
New Project Aims to Predict South Asian Floods
How Shifting Storm Tracks Are Amplifying Climate Change
What Would Pristine Air Mean for the Climate?


Ben Cook, a climatologist affiliated with NASA’s Goddard Institute for Space Studies (GISS) and Columbia University’s Lamont-Doherty Earth Observatory in New York City, highlighted new research that indicates the ancient Meso-American civilizations of the Mayans and Aztecs likely amplified droughts in the Yucatán Peninsula and southern and central Mexico by clearing rainforests to make room for pastures and farmland.

Converting forest to farmland can increase the reflectivity, or albedo, of the land surface in ways that affect precipitation patterns. “Farmland and pastures absorb slightly less energy from the sun than the rainforest because their surfaces tend to be lighter and more reflective,” explained Cook. “This means that there’s less energy available for convection and precipitation.”

NASA, December 2011