The silence you may have heard since our last post was the sound of microscope lights flickering, measuring stages gliding, brains grinding, numbers crunching, and poi dogs pondering. We wrapped up all planned field work last summer for our research grant on climate, fire, and forest history in Mongolia. We have transitioned from the field-intensive portion of the grant to the data and publication phase of the scientific process. We have presented research in various meetings and settings and have earnestly begun to put our findings to our peers to begin the publication process. We are also transitioning to a new vein of research in Mongolia that gets to the title of this blog. It has been a long time coming.
First, Dr. Amy Hessl was inspired by the forest in transition on Solongotyin Davaa. This is the famous forest where global warming was first reported in Mongolia. High elevation forests are rare to burn. So, the thought that a landscape with wood that has been on the forest floor for more than 100o years became an important part of Amy’s summary on “Pathways for climate change effects on fire: Models, data, and uncertainties“.
Next, Amy led a slew of us in a publication summarizing our initial findings of fire history from the northern edge of the Gobi Steppe to Mongolia’s border with Russia near Sükhbaatar City. With the glaring exception on Bogd Uul, this paper, “Reconstructing fire history in central Mongolia from tree-rings“, gives a quick glimpse into the fairly persistent fire regime across central Mongolia over the last 280-450 years.
NPR recently finished a series of reports on the environmental and cultural transitions currently happening in Mongolia as a result of climate change and the massive mining boom underway. The post that caught our attention was the one on “Mongolia’s Dilemma: Who Gets The Water?” Water has been a focus or the Mongolian-American Tree-Ring Project (MATRIP) since the beginning (see MATRIP’s major publications on this subject here, here (get the streamflow data here), here, here). So, we are happy to announce that this rich vein of research has continued with the fire history research grant by first filling an important gap in the MATRIP network and then having several manuscripts on this subject in revision or review.
One paper that we are quite excited about is an analysis of drought variability across Mongolia’s ‘Breadbasket’. We were taken aback in throughout the last three field seasons by the large-scale revitalization of Mongolia’s agricultural sector. It was surprising to see center-pivot irrigation and large tracts of fields in northern Mongolia. This cultural change is intended to transition Mongolia towards agricultural independence for its growing population. Our analysis highlights important differences in drought variation for the eastern and western portions of the breadbasket region. Stay tuned!
Finally, we are headed back to Mongolia this summer to begin pilot work on new research currently funded by the Lamont Climate Center, The National Geographic Society, and West Virginia University. As hinted in our last post, we will begin field work to determine if there was a warmer and wetter climate during the rise of Chinggis Khaan’s Mongol Empire.
Really – stay tuned!