Spelling suggestions: "subject:"soilmoisture"" "subject:"highmoisture""
481 |
SAR remote sensing of soil MoistureSnapir, Boris 12 1900 (has links)
Synthetic Aperture Radar (SAR) has been identified as a good candidate to
provide high-resolution soil moisture information over extended areas. SAR data
could be used as observations within a global Data Assimilation (DA) approach
to benefit applications such as hydrology and agriculture. Prior to developing an
operational DA system, one must tackle the following challenges of soil moisture
estimation with SAR: (1) the dependency of the measured radar signal on both soil
moisture and soil surface roughness which leads to an ill-conditioned inverse problem,
and (2) the difficulty in characterizing spatially/temporally surface roughness of
natural soils and its scattering contribution.
The objectives of this project are (1) to develop a roughness measurement method
to improve the spatial/temporal characterization of soil surface roughness, and (2)
to investigate to what extent the inverse problem can be solved by combining multipolarization,
multi-incidence, and/or multi-frequency radar measurements.
The first objective is achieved with a measurement method based on Structure
from Motion (SfM). It is tailored to monitor natural surface roughness changes which
have often been assumed negligible although without evidence.
The measurement method is flexible, a.ordable, straightforward and generates
Digital Elevation Models (DEMs) for a SAR-pixel-size plot with mm accuracy. A
new processing method based on band-filtering of the DEM and its 2D Power Spectral
Density (PSD) is proposed to compute the classical roughness parameters. Time
series of DEMs show that non-negligible changes in surface roughness can happen
within two months at scales relevant for microwave scattering.
The second objective is achieved using maximum likelihood fitting of the Oh
backscattering model to (1) full-polarimetric Radarsat-2 data and (2) simulated
multi-polarization / multi-incidence / multi-frequency radar data.
Model fitting with the Radarsat-2 images leads to poor soil moisture retrieval
which is related to inaccuracy of the Oh model. Model fitting with the simulated
data quantifies the amount of multilooking for di.erent combinations of measurements
needed to mitigate the critical e.ect of speckle on soil moisture uncertainty.
Results also suggest that dual-polarization measurements at L- and C-bands are a
promising combination to achieve the observation requirements of soil moisture.
In conclusion, the SfM method along with the recommended processing techniques
are good candidates to improve the characterization of surface roughness. A
combination of multi-polarization and multi-frequency radar measurements appears
to be a robust basis for a future Data Assimilation system for global soil moisture
monitoring.
|
482 |
CARBON-DIOXIDE AND PH RELATION DURING THE DRYING CYCLE OF CALCAREOUS SOILSNiebla, Elvia Elisa January 1979 (has links)
No description available.
|
483 |
The osmotic values of certain native forage plants under different climatic and soil conditions in Southern ArizonaLove, L. D. (Lawrence Dudley), 1909- January 1934 (has links)
No description available.
|
484 |
GEOGRAPHIC VARIABILITY OF CREOSOTEBUSH (LARREA TRIDENTATA (D.C.) COV.) INRESPONSE TO MOISTURE AND TEMPERATURE STRESSSaunier, Richard E. January 1967 (has links)
No description available.
|
485 |
Diagnostics and Generalizations for Parametric State EstimationNearing, Grey Stephen January 2013 (has links)
This dissertation is comprised of a collection of five distinct research projects which apply, evaluate and extend common methods for land surface data assimilation. The introduction of novel diagnostics and extensions of existing algorithms is motivated by an example, related to estimating agricultural productivity, of failed application of current methods. We subsequently develop methods, based on Shannon's theory of communication, to quantify the contributions from all possible factors to the residual uncertainty in state estimates after data assimilation, and to measure the amount of information contained in observations which is lost due to erroneous assumptions in the assimilation algorithm. Additionally, we discuss an appropriate interpretation of Shannon information which allows us to measure the amount of information contained in a model, and use this interpretation to measure the amount of information introduced during data assimilation-based system identification. Finally, we propose a generalization of the ensemble Kalman filter designed to alleviate one of the primary assumptions - that the observation function is linear.
|
486 |
A quantitative measure of the effect of the soil moisture and atmospheric moisture on the growth of treesMace, Arnett C. January 1962 (has links)
No description available.
|
487 |
Simultaneous heat balance and soil moisture measurements in Walnut GulchRiley, James J. January 1963 (has links)
No description available.
|
488 |
The climate of the Rupununi Savannas : a study in ecological climatology.Frost, David B. January 1966 (has links)
The intent of this thesis is to set out new data relating to the climate of the savanna in the Rupununi district of Guyana, and to comment thereon with reference to the causes and continuing existence of that savanna. To indicate the significance of the data and the pertinence of the comments it will be necessary to review recent discussion of the nature and causes of savanna in general. [...]
|
489 |
A Multitemporal Analysis of Georgia's Coastal Vegetation, 1990-2005Breeden, Charles, III F 17 April 2008 (has links)
Land and vegetation changes are part of the continuous and dynamic cycle of earth system variation. This research examines vegetation changes in the 21-county eco-region along coastal Georgia. The Advanced Very High Resolution Radiometer (AVHRR) with Normalized Difference Vegetation Index (NDVI) data is used in tandem with a Principal Component Analysis (PCA) and climatic variables to determine where, and to what extent vegetation and land cover change is occurring. This research is designed around a 16 year time-series from 1990-2005. Findings were that mean NDVI values were either steady or slightly improved, and that PC1 (Healthiness) and PC2 (Time-Change) explained nearly 99 percent of the total mean variance. Healthiness declines are primarily the result of expanding urban districts and decreased soil moisture while increases are the results of restoration, and increased soil moisture. This research aims to use this analysis for the assessment of land changes as the conduit for future environmental research.
|
490 |
Suitability of Canadian-bred and Native Plant Species for Extensive Green Roofs in Northern Nova ScotiaGrant, Jason J W 20 February 2013 (has links)
Research was conducted to determine individual suitability of native and Canadian-bred selected plants in terms of growth and survivability for local extensive green roofs. The experiment was single-factor (species) with 12 levels (two Sedum spp. [controls]; 10 Canadian-bred or native plant species) in a randomized complete block design with three blocks. Variables measured were percent survival and cover, height, fresh and dry weights, stomatal conductance, transpiration, photosynthetic rate, soil temperature, soil moisture, and reflectance. Artemisia stelleriana contributed more to cooling through transpiration than Sedum floriferum, and maintained similar soil moisture to Sedum acre. Lotus corniculatus was similar to the controls in photosynthetic rate and had higher reflectance than Sedum acre in July. With high biomass and photosynthetic rates, Aster novi-belgii may contribute more to carbon sequestration and insulation than the controls. Artemisia stelleriana , Lotus corniculatus, and Aster novi-belgii are suitable species for extensive green roofs in northern Nova Scotia.
|
Page generated in 0.0576 seconds