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Siberia 2012 – Embenchime River Expedition: Siberia 2012 – Embenchime River Expedition: Introduction

July 9th, 2012 by Joanne Howl

To many people, the Arctic is an almost unimaginably remote area at the end of the Earth – more a land of fable and fantasy than a real part of the everyday world. Most people have very little day-to-day connection with the forests, the fields, and the people who are all part of the vast boreal ecosystem. Yet, in a very real way, the health of every person and every ecosystem on Earth is linked to the health Arctic. We are all connected to the Arctic – and that connection is carbon.

A typical larch forest in summer. The boreal ecosystem encompasses a vast region along the northern edges of North America, Europe, and Asia, including the Arctic Circle. The boreal forest covers about 20 million square km (more than 7.7 million square miles) of the Earth’s surface. In Russia, larch is the dominant tree species in the taiga, covering some 278 million ha, or 42% of Russian forests, and occupying about 70% of the permafrost areas in Siberia.

It is because of this vital connection to the Earth’s health – the carbon stored in the frozen soil and the vast forestlands of the Arctic region – that it is imperative to understand the boreal ecosystem. As a carbon sink, the boreal region helps stabilize the Earth’s climate by keeping carbon in storage, and out of the atmosphere. But a warming climate may bring increased fires to the forest, and rapid decomposition of thawing carbon-rich soil. Both burning and decomposition release carbon into the atmosphere – which, in turn, is expected to increase warming.

Driven by the desire to learn more about a vital, yet scantily studied, region, a dedicated team of scientists from NASA and Russia’s Academy of Science are embarking on a two week expedition in the remote boreal forests of northern Siberia. The international team, led by Jon Ranson, Chief of the Biospheric Sciences Branch at NASA’s Goddard Space Flight Center and Slava Kharuk of the Sukachev Forest Institute, will hop a helicopter in Tura, and then disembark on the banks of the remote Embenchime (Em- bem- chee-may) River in far northern Siberia.

They will be studying the larch forests (taiga) of the region to broaden the understanding of the Siberian larch forest in many ways, including validating measurements of forest height, structure and biomass which have already been made by the ICESat satellite’s GLAS instrument, looking at the fire history and fire-return intervals in the region, and making visual observations to collect information on any changes that may be occurring due to regional warming, including tree heights, growth patterns, types of trees which grow there, and the location of the taiga-tundra ecotone – the place where forest gives way to scrubby grassland.

Another, very important, reason for this expedition is to pave the way for use of a unique, well-tested, yet little utilized instrument package, so that it can be flown over these same forests over the next two years to collect high-resolution, detailed data on forest structure. Known as the Goddard Lidar, Hyperspectral and Thermal (G-LiHT) system, it contains imaging lidar, visible and near infrared hyperspectral and thermal capabilities. This instrument package is small enough and sturdy enough to fit aboard Russian aircraft, and has the potential to characterize the forest with more accuracy that has been available up to this time.

Dr. Jon Ranson (left) and Dr. Slava Kharuk (right) have each spent their careers studying the boreal forests of Siberia, and have collaborated for over two decades. The Embenchime Expedition marks their 10th joint scientific foray into the remote forests of Sibera. This picture was taken at the Krasnoyarsk airport in 2007. Paul Montesano, in green, participated in the 2007 expedition but was not able to travel with the team in 2012.

The Arctic Carbon Connection
The boreal ecosystem encompasses a vast region along the northern edges of North America, Europe, and Asia, including the Arctic Circle. Named after Boreas, the Greek god of the north wind, the world’s boreal forest is huge – almost 20 million square kilometers (more than 7.7 million square miles), or 29 times the state of Texas. In Russia, larch is the dominant tree species in the taiga, covering some 278 million ha, or 42% of Russian forests, and occupying about 70% of the permafrost areas in Siberia.

The roots of the taiga’s forests grow in a unique soil – one which is almost entirely made up of carbon. In much of the boreal biome, this carbon-rich soil is comprised of thick layers of peat – dead plant matter that decomposes very slowly or not at all. A meter or so below the moss-covered surface, the soil is frozen – a state the both stabilizes the carbon stores of the soil and slows the growth of forest trees.

Between the trees and the frozen soil, the Arctic region holds a vast amount of carbon, tucking it away and keeping it out of the atmosphere. In fact, Scientists estimate that while the boreal forest occupies about 21% of the Earth’s forested land surface and contains 13% of all the carbon stored in biomass (or living matter), it holds about 43% of all of the world’s carbon that is stored in soil.

Once released, carbon becomes a greenhouse gas (carbon dioxide), which contributes strongly to global warming. In a warming Arctic, peat soils begin to thaw, releasing both carbon and methane (another powerful greenhouse gas). Also, dead trees, which currently stand literally “frozen” in time, undecomposed over hundreds of years, will begin to decompose as temperatures rise. Also, as the taiga dries in warmer weather, the incidence of fires are predicted to increase. Both fire and decomposition release carbon, increasing the concentration of greenhouse gases.

Because the Arctic holds so much carbon, it is known as a carbon “sink”. As long as the Arctic stays cold, and the forests of the region continue to absorb carbon emitted by other sources (particularly human activity) our climate in our home latitudes can also remain relatively stable. Should the Arctic thaw, however, the release of both carbon and methane can heavily contribute to a warming world.

Warmth has already come to much of the Arctic. In the last 40 years, scientists have reported that the average temperatures have increased over these regions by as much as 1.25°C per decade. In northern Siberia, average temperatures have risen 1 to 3°C (3 to 5°F) over the past 30 years, whereas the worldwide average increase in that time is 0.6°C (1°F).

Oblique Google Earth map of study sites (red boxes) in Arctic Siberia. Field measurements were acquired by the team along the Kochechum River in 2007 and Kotuykan-Kotuy Rivers (north box) in 2008. This expedition leaves from Tura, in the south, and will travel 480 km along the Embenchime River from near the Arctic Circle to Tura.

Back to the Future
The NASA-Sukachev scientists have been intensely interested in Siberia’s boreal ecosystem for decades. Dr. Jon Ranson and Dr. Slava Kharuk have both committed their entire careers to improving understanding of the region, and have partnered in their study since 1991. The Embenchime River Expedition will mark their 10th expedition together in the remote forests of Siberia.

In 2007 and 2008, the expeditions were similar, traveling for weeks to measure forests on the banks of the Kochechum (2007) and the Kotuykan (2008) Rivers. The Embenchime is one of the major tributaries to the Kochechum and flows one valley to the south of it, so this expedition returns to similar conditions as the team experienced in 2007.

The waters of both the Kochechum and Embenchime come primarily from summer melt of winter ice and snowfields. Even in high summer, the rivers are icy cold, and sometimes unpredictable. Heavy rains upstream can swell the rivers with surprising swiftness, causing rapidly rising waters to soak a campsite placed too close to the river. The waters can also become dangerously fast with no notice, so the scientists must sport life jackets at all time when on the river.

An expedition in Siberia is hard work, under strenuous and dangerous conditions, with hordes of mosquitoes buzzing about. Despite the adversity, these two scientists have returned to these forests, again and again, for over two decades – and plan to return as long as they are able. It’s not sheer adventure that brings them back to these beautiful but harsh conditions, again and again. They are driven by the need to learn more about the boreal ecosystem and its integral role in the health of the Earth. From these ongoing studies, these scientists hope to help the Earth, and all of her inhabitants, have a more habitable future.

Siberia 2012 – Embenchime River Expedition: Siberia 2012: Embenchime River Expedition – Biographies

July 8th, 2012 by Joanne Howl

Dr. Jon Ranson is an earth scientist specializing in radar and lidar remote sensing of forests. He uses these tools for studying vegetation type and biomass in ecosystem research at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. He also serves as the Chief of Goddard’s Biospheric Science Laboratory, which is advancing the use of satellite technology to study the carbon cycle and terrestrial ecosystems. Dr. Ranson has participated in numerous field campaigns in the United States, Canada and Siberia to improve our ability to measure and monitor vegetated ecosystems from space. He enjoys hiking, birding, music and outdoor cooking.

Dr. Vyacheslav Kharuk, a forest ecologist, is Head of Forest Ecology and Monitoring Branch, Sukachev Forest Institute Siberian Branch of the Russian Academy of Science, in Krasnoyarsk, Siberia and Head of GIS Chair at Siberian Federal University. He has collaborated on several NASA- supported projects including projects in Maine, Canada and Siberia with Dr. Ranson and other NASA and USDA Forest Service scientists over the past several years. Dr. Kharuk leads the field and remote-sensing data activities at the Sukachev Institute and collaborates in data analysis research at NASA GSFC.

Dr. Guoqing Sun is a Research Professor at the University of Maryland-College Park, and is also affiliated with NASA’s Goddard Space Flight Center Biospheric Sciences Branch. He has been involved in research on remote sensing and GIS applications since the early 1980s , and has worked as a principal researcher and investigator in various NASA programs. His speciality is in radar backscatter and lidar waveform models and applications of multi-sensor (lidar, radar and passive optical sensors) data in forest ecosystem studies.

 

Dr. Sergei Im is a scientist at the V. N. Sukachev Institute of Forests, Siberian Branch of the Russian Academy of Science in Krasnoyarsk, Siberia. He completed his undergraduate Studies at Krasnoyarsk University in 2001 and completed his post-graduate studies at the V. N. Sukachev Institute. He is author and co-author of many scientific papers that have been published in Russian and International journals. His special interests are informatics such as GIS. Dr. Im is a skilled computer programmer. He has a particular interest in microwave and optical remote sensing for analysis of land cover dynamics.

 

Dr. Ross Nelson is a physical scientist who works for the Biospheric Branch of the NASA Goddard Space Flight Center in Greenbelt, Maryland. He completed his B.S. in Forestry at the University of Maine, Orono, his Master’s in Forestry/Remote Sensing at Purdue University and earned his Ph.D. in Forestry/Biometrics at Virginia Polytechnic Institute and State University. He participates in several areas of research. One important area is the use of airborne laser data to characterize the forest canopy and estimate forest biomass, volume and carbon. He is also working to use moderate and high-resolution satellite data to monitor tropical and subtropical forest conversion. Ross is also developing statistical and image processing procedures for continental and sub-continental resource assessment using satellite imagery.

 

Pavel Oskorbin is a scientist at the V.N. Sukachev Institute of Forests, Siberian Branch of the Russian Academy of Science in Krasnoyarsk, Siberia. He is a veteran of several field expeditions in the Siberian forest, working with field studies as well as logistics. Pasha was born on the coast of Lake Baikal lake in 1980. He graduated from Krasnoyarsk State Technological University. Now, he is working in V. N. Sukachev Institute of Forest SB RAS as a researcher with PhD. His field of interest is forest stand structural dynamics. He is the participant of a number of international expeditions.

Dr. Joanne Howl received her Doctor of Veterinary Medicine from the University of Tennessee College of Veterinary Medicine, Knoxville, Tennessee in 1987. She has practiced clinical veterinary medicine, worked in veterinary emergency response and is a writer and editor in the pet health and science fields. Currently she is employed as a Technical Writer for Sigma Space. This is her sixth year blogging for the Earth Observatory in support of NASA field campaigns.  She is the US based contact for the NASA Expedition Team, and communicates via satellite phone and email while the Team is in field, and shares their story with the reader.

Soil Moisture Active Passive (SMAP): Notes from the Field – Week 4

July 5th, 2012 by Brian Campbell

Grant Wiseman
Agriculture and Agri-Food Canada

Another hot and dry week here in southern Manitoba has us missing the rain just a little bit. We have experienced a very nice dry down cycle in weeks 3 and 4 after a wet up period initially in weeks 1 and 2. By all accounts this will contribute to a very informative and descriptive dataset.

Some sandy loam soils have approached zero volumetric moisture levels, while many clay soils remain high at 25 or 30 percent but it has become rather difficult to insert moisture probes. Even morning dew levels have subsided. Dare I say, “Let it rain?”

Field crews are well into their groove with many not requiring the use of GPSs or maps for navigation any longer. On a much-deserved scheduled down day some team members took in the Canada Day festivities and fireworks on July 1st at Assiniboine Park or The Forks.

We’re two thirds of the way through and going strong, looking forward to the home stretch!

 

For more information, visit the SMAP Blogs from the Field page.

Soil Moisture Active Passive (SMAP): Musings from SMAPVEX12 Winnipeg

July 3rd, 2012 by Brian Campbell

Narendra Das
Jet Propulsion Laboratory

I am signing off from SMAPVEX12 at Winnipeg with good vibes, pleasant memories and expectation that this will be a very successful campaign. I hope that, like me, most of my teammates have learnt substantially about the study area and had a great field sampling experience, and have also made many good friends during interactions and group dinners.

I conducted crop structure sampling of various crops (corn, beans, canola, wheat, and pasture) for the last one month and witnessed the growth spurt in crops within the one month span. Even though I knew about crop responses to weather variables I was amazed to see such a rapid response of crop growth to conducive environment conditions, especially for canola and corn.

Dr. Tsang, Dr. Jackson, Narendra, and Sab

Corn plants on 06-09-2012

Corn plants on 06-30-2012

 

For more information and pictures, visit the SMAP Blogs from the Field page.