Go Iwahana, a postdoctoral researcher at the UAF
International Arctic Research Center (IARC) is especially interested in this
topic and has been working this week to install a network of soil moisture
probes across the Barrow Environmental Observatory (BEO). These probes are
commercially available and, once connected to a small data logger, can record
information on soil temperature and moisture for months at a time. Go plans to
use data from this network to evaluate relationships between plot-scale data
and that coming from the Soil Moisture Active Passive (SMAP) satellite. The
intended goal of SMAP is to provide global measurements of soil moisture and
its freeze/thaw state. These measurements will be used to enhance understanding
of processes that link the water, energy, and carbon cycles, and to extend the
capabilities of weather and climate prediction models. SMAP is a directed
mission of NASA (https://smap.jpl.nasa.gov/)
and is managed by the Jet Propulsion Laboratory.
Characterized by vast amounts of carbon stored in permafrost and a rapidly evolving landscape, the Arctic is an important focal point for the study of climate change. These are sensitive systems, yet the mechanisms responsible for those sensitivities remain poorly understood and inadequately represented in Earth System Models. The NGEE Arctic project seeks to reduce uncertainty in climate prediction by better understanding critical land-atmosphere feedbacks in terrestrial ecosystems of Alaska.
Monday, September 1, 2014
NGEE Arctic Scientist Links Plot Scale and Satellite Scale Measurements of Soil Moisture…
Much of what the NGEE Arctic team does is directed at
gaining fundamental knowledge of processes that control the water, energy, and
carbon cycles in tundra ecosystems. This means that members of the team are in
the field and laboratory gathering data and sharing that information with our
modeling colleagues. We also have an interest in linking our field studies to
larger scale information coming from satellites in what if often referred to as
scaling. That is, how do small-scale measurements made in the field relate to
larger scale properties and processes estimated from remote sensing platforms?