Constraining ecosystem processes from tower fluxes and atmospheric profiles.

The planetary boundary layer (PBL) provides an important link between the scales and processes resolved by global atmospheric sampling/modeling and site-based flux measurements. The PBL is in direct contact with the land surface, both driving and responding to ecosystem processes. Measurements within the PBL (e.g., by radiosondes, aircraft profiles, and flask measurements) have a footprint, and thus an integrating scale, on the order of 1-100 km. We use the coupled atmosphere-biosphere model (CAB) and a Bayesian data assimilation framework to investigate the amount of biosphere process information that can be inferred from PBL measurements. We investigate the information content of PBL measurements in a two-stage study. First, we demonstrate consistency between the coupled model (CAB) and measurements, by comparing the model to eddy covariance flux tower measurements (i.e., water and carbon fluxes) and also PBL scalar profile measurements (i.e., water, carbon dioxide, and temperature) from Canadian boreal forest. Second, we use the CAB model in a set of Bayesian inversions experiments using synthetic data for a single day. In the synthetic experiment, leaf area and respiration were relatively well constrained, whereas surface albedo and plant hydraulic conductance were only moderately constrained. Finally, the abilities of the PBL profiles and the eddy covariance data to constrain the parameters were largely similar and only slightly lower than the combination of both observations.

How much energy do barn owls (Tyto alba) save by roosting?

(1) The energy savings associated with the roosting behaviour of barn owls (Tyto alba) were determined with a biophysical model using measurements of microclimate from a roost and nest site in SW Scotland (55 degrees 10' N 3 degrees 12' W) from April 1991-March 1992. (2) The roost building provided complete shelter from wind and precipitation. Air temperature inside the roost building was 1.4 degrees C greater than ambient and matched the seasonal change in temperature. Air temperature inside the nest box was on average only 0.8 degrees C greater than ambient but was 2-3 degrees C warmer when adults and chicks were in the nest during the breeding season. (3) Estimated metabolic heat production was significantly different between locations and averaged 67.9, 68.1, 75.5 and 84.2Wm(-2) for a barn owl roosting in the building, nest box, spruce tree and in the open, respectively. At night metabolic heat production was greater by 4-12% compared with daytime, depending on location. (4) Heat loss was 30% greater in winter months than in the summer in all locations. By roosting in the building an owl would make savings of 21.6Wm(-2) in March but only 12.9Wm(-2) in August. In a tree roost a barn owl would save 11.8Wm(-2) in March and 5.8Wm(-2) in August. (5) Barn owls were estimated to reduce metabolic heat production by 19% by roosting in the building and by 10% by roosting in a tree. In the building and tree savings of 21 and 9% occurred during the day compared with 17 and 12% at night. (6) Metabolic savings were strongly dependent on weather conditions with average metabolic savings of 26% occurring in wet and windy conditions compared with only 12% on dry-calm days. Maximum savings of 29-36% occurred on wet days. (7) Barn owls appear to compensate for high metabolic demands for heat production by taking advantage of better thermal conditions within buildings, especially during the day when metabolic savings are greatest.

Estimating mean monthly incident solar radiation on horizontal and inclined slopes from mean monthly temperatures extremes.

Although satellite-borne sensors are now available to estimate cloud cover and incoming short-wave radiation across the Earth's surface, the study of climatic variation and its impact on terrestrial and marine ecosystems involves historical analyses of data from networks of weather stations that only record extremes in temperatures and precipitation on a daily basis. Similarly, when projections are made with global atmospheric circulation models, the spatial resolution of predicted radiation is too coarse to incorporate the effects of heterogeneous topography. In this paper, we review the development and set forth a set of general equations that allow both diffuse and direct solar radiation to be estimated for each month on the basis of mean daily maximum and minimum temperatures, latitude, elevation, slope, and aspect. Adjustments for differences in slope, aspect, and elevation are made by varying the fraction of diffuse and direct solar beam radiation. To test the equations on various slopes and under different climatic conditions, we drew on highquality radiation data recorded at a number of sites on three continents. On horizontal surfaces the set of equations predicted both direct and diffuse components of solar radiation within 1%-7% of recorded values. On slopes, estimates of monthly mean solar radiation were with 13% of observed values with a mean error of less than 2 MJ m(-2) day(-1) over any given month.

Deposition of atmospheric ammonia to moorlands.

Micrometeorological methods were applied to measure fluxes of atmospheric ammonia (NH3) to moorlands. Measurements were made in a wide variety of surface conditions and included both Calluna vulgaris (L.) Hull and Eriophorum vaginatum L. dominated sites. NH3 was found to deposit rapidly to all the sites investigated, providing large deposition velocities (Vd, typically 10-40 mm s(-1)) and usually minimal surface resistances (rc). A small number of measurements were made in frozen conditions and suggest a possible exception to this pattern with mean rc of 50-200 s m(-1). The effect of vegetation drying was also investigated and a possible increase in rc observed, though this was small (< 10 s m(-1)). The results are interpreted in terms of the processes controlling exchange; it is shown that NH3 deposition is predominantly to the leaf surfaces and that the net NH3 compensation point approaches zero. Annual estimates show that dry deposition of NH3 is a major source of atmospheric nitrogen to moorland ecosystems. For two typical UK sites subject to background air concentrations, NH3 dry deposition is of similar magnitude to equivalent NH4+ inputs in wet deposition. In the vicinity of emission sources, NH3 dry deposition is expected to dominate inputs of atmospheric nitrogen.