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Keywords = WSMN

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18 pages, 4662 KiB  
Article
SMAP Soil Moisture Product Assessment over Wales, U.K., Using Observations from the WSMN Ground Monitoring Network
by Dileep Kumar Gupta, Prashant K. Srivastava, Ankita Singh, George P. Petropoulos, Nikolaos Stathopoulos and Rajendra Prasad
Sustainability 2021, 13(11), 6019; https://doi.org/10.3390/su13116019 - 27 May 2021
Cited by 4 | Viewed by 2553
Abstract
Soil moisture (SM) is the primary variable regulating the soil temperature (ST) differences between daytime and night-time, providing protection to crop rooting systems against sharp and sudden changes. It also has a number of practical applications in a range of disciplines. This study [...] Read more.
Soil moisture (SM) is the primary variable regulating the soil temperature (ST) differences between daytime and night-time, providing protection to crop rooting systems against sharp and sudden changes. It also has a number of practical applications in a range of disciplines. This study presents an approach to incorporating the effect of ST for the accurate estimation of SM using Earth Observation (EO) data from NASA’s SMAP sensor, one of the most sophisticated satellites currently in orbit. Linear regression analysis was carried out between the SMAP-retrieved SM and ground-measured SM. Subsequently, SMAP-derived ST was incorporated with SMAP-derived SM in multiple regression analysis to improve the SM retrieval accuracy. The ability of the proposed method to estimate SM under different seasonal conditions for the year 2016 was evaluated using ground observations from the Wales Soil Moisture Network (WSMN), located in Wales, United Kingdom, as a reference. Results showed reduced retrieval accuracy of SM between the SMAP and ground measurements. The R2 between the SMAP SM and ground-observed data from WSMN was found to be 0.247, 0.183, and 0.490 for annual, growing and non-growing seasons, respectively. The values of RMSE between SMAP SM and WSMN observed SM are reported as 0.080 m3m−3, 0.078 m3m−3 and 0.010 m3m−3, with almost zero bias values for annual, growing and non-growing seasons, respectively. Implementation of the proposed scheme resulted in a noticeable improvement in SSM prediction in both R2 (0.558, 0.440 and 0.613) and RMSE (0.045 m3m−3, 0.041 m3m−3 and 0.007 m3m−3), with almost zero bias values for annual, growing and non-growing seasons, respectively. The proposed algorithm retrieval accuracy was closely matched with the SMAP target accuracy 0.04 m3m−3. In overall, use of the new methodology was found to help reducing the SM difference between SMAP and ground-measured SM, using only satellite data. This can provide important assistance in improving cases where the SMAP product can be used in practical and research applications. Full article
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Figure 1

Figure 1
<p>(<b>a</b>) Overview of the locations on which the WSMN experimental sites are installed to acquire SM, ST and ancillary data. Examples of images of the sites from: (<b>b</b>) Penglais, (<b>c</b>) Pwllpeiran, (<b>d</b>) Cae-Canol, and (<b>e</b>) Comins-Coch. Figure is adopted from [<a href="#B28-sustainability-13-06019" class="html-bibr">28</a>].</p>
Full article ">Figure 2
<p>Temporal variation of SMAP and WMSN soil moisture. (<b>a</b>) Annual temporal variation of SM. (<b>b</b>) Temporal variation of SM during the growing season. (<b>c</b>) Temporal variation of SM during the non-growing season.</p>
Full article ">Figure 3
<p>Temporal variation of SMAP and WMSN soil temperature. (<b>a</b>) Annual temporal variation of soil temperature. (<b>b</b>) Temporal variation of soil temperature during the growing season. (<b>c</b>) Temporal variation of soil temperature during the non-growing season.</p>
Full article ">Figure 4
<p>The temporal variation soil moisture, soil temperature, MODIS evapotranspiration, and MODIS NDVI: (<b>a</b>) for SMAP; (<b>b</b>) for WSMN.</p>
Full article ">Figure 5
<p>Scatter plots between (<b>a</b>) WSMN ST and SMAP ST, and (<b>b</b>) WSMN SM and SMAP SM for annual datasets.</p>
Full article ">Figure 6
<p>Scatter plots between (<b>a</b>) WSMN ST and SMAP ST, and (<b>b</b>) WSMN SM and SMAP SM for growing season datasets.</p>
Full article ">Figure 7
<p>Scatter plots between (<b>a</b>) WSMN ST and SMAP ST, and (<b>b</b>) WSMN SM and SMAP SM for non-growing season datasets.</p>
Full article ">Figure 8
<p>Scatter plots between retrieved soil moisture using the SMAP datasets (SM and ST) and observed WSMN SM data for (<b>a</b>) annual, (<b>b</b>) growing season, and (<b>c</b>) non-growing season.</p>
Full article ">Figure 9
<p>Spatial soil moisture maps for the SMAP SM and retrieved SM using average SM values for annual, growing and non-growing seasons.</p>
Full article ">
2184 KiB  
Article
An Operational In Situ Soil Moisture & Soil Temperature Monitoring Network for West Wales, UK: The WSMN Network
by George P. Petropoulos and Jon P. McCalmont
Sensors 2017, 17(7), 1481; https://doi.org/10.3390/s17071481 - 23 Jun 2017
Cited by 26 | Viewed by 6007
Abstract
This paper describes a soil moisture dataset that has been collecting ground measurements of soil moisture, soil temperature and related parameters for west Wales, United Kingdom. Already acquired in situ data have been archived to the autonomous Wales Soil Moisture Network (WSMN) since [...] Read more.
This paper describes a soil moisture dataset that has been collecting ground measurements of soil moisture, soil temperature and related parameters for west Wales, United Kingdom. Already acquired in situ data have been archived to the autonomous Wales Soil Moisture Network (WSMN) since its foundation in July 2011. The sites from which measurements are being collected represent a range of conditions typical of the Welsh environment, with climate ranging from oceanic to temperate and a range of the most typical land use/cover types found in Wales. At present, WSMN consists of a total of nine monitoring sites across the area with a concentration of sites in three sub-areas around the region of Aberystwyth located in Mid-Wales. The dataset of composed of 0–5 (or 0–10) cm soil moisture, soil temperature, precipitation, and other ancillary data. WSMN data are provided openly to the public via the International Soil Moisture Network (ISMN) platform. At present, WSMN is also rapidly expanding thanks to funding obtained recently which allows more monitoring sites to be added to the network to the wider community interested in using its data. Full article
Show Figures

Figure 1

Figure 1
<p>(<b>a</b>) Overview of the locations on which the WSMN experimental sites are installed to acquire SM, ST, and ancillary data. Examples of images of the sites from: (<b>b</b>) Penglais, (<b>c</b>) Pwllpeiran, (<b>d</b>) Cae-Canol (<b>e</b>) Comins-Coch.</p>
Full article ">Figure 2
<p>Time series of SSM at 5 cm depth from the soil surface layer measured at the WSMN experimental sites from their individual installation dates to the present.</p>
Full article ">Figure 3
<p>Time series of ST at 5 cm depth from the soil surface layer measured at the WSMN experimental sites from their individual installation dates to the present.</p>
Full article ">Figure 4
<p>Monthly totals of rainfall measurements from the WSMN sites collected between 2011 and 2016.</p>
Full article ">Figure 5
<p>Summarised statistics of the WSMN data usage for the period 1 July 2016 to December 2016.</p>
Full article ">
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