|
Summary
Net ecosystem productivity (NEP) is a critical
characteristic of terrestrial ecosystem response to environment.
Processes controlling NEP operate on a variety of temporal
and spatial scales and are influenced by physiology, allocation,
forest development, climate and disturbance. We are simulating
NPP and NEP in Oregon and Washington using a combination of
remote sensing, site data, and process models. Model outputs
are being tested using detailed ecosystem studies at intensive
sites, more basic ecological measurements at other existing
intensive sites, and survey data from Forest Health Monitoring
(FHM), Forest Inventory and Analysis (FIA) plots, and Current
Vegetation Survey (CVS) plots. In spatially explicit applications,
we are predicting and evaluating forest productivity for an
east-west longitudinal swath along a steep climatic gradient
through central Oregon from the coast to the semi-arid east
side of the Cascade Mountains, and a north-south latitudinal
swath from the southern Oregon border to southern Washington.
These swaths encompass:
- Six Oregon Transect Ecosystem Research (OTTER) project
sites across central OR.
- Two tower flux sites in young and old ponderosa pine (green
stars at Metolius).
- Two tower flux sites in young and old Douglas-fir/hemlock
in WA (green star at Wind River).
- Long-term vegetation plots at HJ Andrews LTER.
- Cascade Head Experimental Forest.
- FHM, FIA, CVS survey data for the PNW region (not shown).
- 36 intensive field sites (at Cascade Head, HJ Andrews,
and Metolius).
- 60 extensive field sites (red triangles).
With BIOME-BGC, a physiologically-based process model, we
are generating current NEP, NPP, and "carbon stress index"
surfaces for the regions for a mean climate year, 1999, and
2000. We will use STANDCARB, an ecosystem process model, to
estimate current carbon pools by accounting for long-term
trends in NEP. BIOME-BGC will be initialized using remote
sensing (Thematic Mapper) estimates of forest cover type,
age class and LAI and soil survey data (FHM, STATSGO). The
model is driven by spatially distributed climate data based
on interpolations of weather station data by the PRISM and
DAYMET models. Remotely sensed variables are validated with
data from intensive sites, FHM, FIA, CVS, and new measurements
in underrepresented forests. Short-term predictions (monthly,
annual) of NEP are validated against tower flux data. Annual
predictions of aboveground NPP and its components are validated
with intensive site measurements of stemwood and litter production.
Predictions of carbon stores are validated with FHM, FIA,
and CVS data. We are evaluating sensitivity of NEP to forest
type, developmental stage, disturbance, and interannual variability
|