2016 ◽  
Vol 182 ◽  
pp. 128-140 ◽  
Author(s):  
Chun-Hsu Su ◽  
Jing Zhang ◽  
Alexander Gruber ◽  
Robert Parinussa ◽  
Dongryeol Ryu ◽  
...  

2016 ◽  
Vol 121 (3) ◽  
pp. 1208-1219 ◽  
Author(s):  
A. Gruber ◽  
C.-H. Su ◽  
W. T. Crow ◽  
S. Zwieback ◽  
W. A. Dorigo ◽  
...  

2016 ◽  
Vol 17 (6) ◽  
pp. 1725-1743 ◽  
Author(s):  
Simon Zwieback ◽  
Chun-Hsu Su ◽  
Alexander Gruber ◽  
Wouter A. Dorigo ◽  
Wolfgang Wagner

Abstract The error characterization of soil moisture products, for example, obtained from microwave remote sensing data, is a key requirement for using these products in applications like numerical weather prediction. The error variance and root-mean-square error are among the most popular metrics: they can be estimated consistently for three datasets using triple collocation (TC) without assuming any dataset to be free of errors. This technique can account for additive and multiplicative biases; that is, it assumes that the three products are linearly related. However, its susceptibility to nonlinear relations (e.g., due to sensor saturation and scale mismatch) has not been addressed. Here, a simulation study investigates the impact of quadratic relations on the TC error estimates [also when the products are first rescaled using the nonlinear cumulative distribution function (CDF) matching technique] and on those by two novel methods. These methods—based on error-in-variables regression and probabilistic factor analysis—extend standard TC by also accounting for nonlinear relations using quadratic polynomials. The relative differences between the error estimates of the ASCAT remotely sensed product by the quadratic and the linear methods are predominantly smaller than 10% in a case study based on remotely sensed, reanalysis, and in situ measured soil moisture over the contiguous United States. Exceptions with larger discrepancies indicate that nonlinear relations can pose a challenge to traditional TC analyses, as the simulations show they can introduce biases of either sign. In such cases, the use of nonlinear methods may complement traditional approaches for the error characterization of soil moisture products.


2015 ◽  
Vol 15 (12) ◽  
pp. 17397-17448 ◽  
Author(s):  
U. Karstens ◽  
C. Schwingshackl ◽  
D. Schmithüsen ◽  
I. Levin

Abstract. Detailed 222Rn flux maps are an essential prerequisite for the use of radon in atmospheric transport studies. Here we present a high-resolution222Rn flux map for Europe, based on a parameterization of 222Rn production and transport in the soil. The 222Rn exhalation rate was parameterized based on soil properties, uranium content, and modelled soil moisture from two different land-surface reanalysis data sets. Spatial variations in exhalation rates are primarily determined by the uranium content of the soil, but also influenced by local water table depth and soil texture. Temporal variations are related to soil moisture variations as the molecular diffusion in the unsaturated soil zone depends on available air-filled pore space. The implemented diffusion parameterization was tested against campaign-based 222Rn profile measurements. Monthly 222Rn exhalation rates from European soils were calculated with a nominal spatial resolution of 0.083° × 0.083° and compared to long-term direct measurements of 222Rn exhalation rates in different areas of Europe. The two realizations of the 222Rn flux map, based on the different soil moisture data sets, both realistically reproduce the observed seasonality in the fluxes but yield considerable differences for absolute flux values. The average 222Rn flux from soils in Europe is estimated to be 10 or 15 mBq m-2 s-1, depending on the soil moisture data set, and the seasonal variations in the two realisations range from 7.1 mBq m-2 s-1 in February to 13.9 mBq m-2 s-1 in August and from 10.8 mBq m-2 s-1 in March to 19.7 mBq m-2 s-1 in July, respectively. This systematic difference highlights the importance of realistic soil moisture data for a reliable estimation of 222Rn exhalation rates.


Eos ◽  
2019 ◽  
Vol 100 ◽  
Author(s):  
Rupesh Shrestha ◽  
Alison Boyer

An integrated data platform harmonizes many disparate soil moisture data sets to better inform disaster response planners, climate scientists and meteorologists, farmers, and others.


2015 ◽  
Vol 15 (22) ◽  
pp. 12845-12865 ◽  
Author(s):  
U. Karstens ◽  
C. Schwingshackl ◽  
D. Schmithüsen ◽  
I. Levin

Abstract. Detailed 222radon (222Rn) flux maps are an essential pre-requisite for the use of radon in atmospheric transport studies. Here we present a high-resolution 222Rn flux map for Europe, based on a parameterization of 222Rn production and transport in the soil. The 222Rn exhalation rate is parameterized based on soil properties, uranium content, and modelled soil moisture from two different land-surface reanalysis data sets. Spatial variations in exhalation rates are primarily determined by the uranium content of the soil, but also influenced by soil texture and local water-table depth. Temporal variations are related to soil moisture variations as the molecular diffusion in the unsaturated soil zone depends on available air-filled pore space. The implemented diffusion parameterization was tested against campaign-based 222Rn soil profile measurements. Monthly 222Rn exhalation rates from European soils were calculated with a nominal spatial resolution of 0.083° × 0.083° and compared to long-term direct measurements of 222Rn exhalation rates in different areas of Europe. The two realizations of the 222Rn flux map, based on the different soil moisture data sets, both realistically reproduce the observed seasonality in the fluxes but yield considerable differences for absolute flux values. The mean 222Rn flux from soils in Europe is estimated to be 10 mBq m−2 s−1 (ERA-Interim/Land soil moisture) or 15 mBq m−2 s−1 (GLDAS (Global Land Data Assimilation System) Noah soil moisture) for the period 2006–2010. The corresponding seasonal variations with low fluxes in winter and high fluxes in summer range in the two realizations from ca. 7 to ca. 14 mBq m−2 s−1 and from ca. 11 to ca. 20 mBq m−2 s−1, respectively. These systematic differences highlight the importance of realistic soil moisture data for a reliable estimation of 222Rn exhalation rates. Comparison with observations suggests that the flux estimates based on the GLDAS Noah soil moisture model on average better represent observed fluxes.


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