scholarly journals Geophysical changes detection by remote sensing in Alaminos River Pangasinan, Philippines

2018 ◽  
Vol 3 (2) ◽  
Author(s):  
Annie Melinda Paz-Alberto 1 ◽  
Edmark P. Bulaong 1 ◽  
Ranilo B. Lao 1 ◽  
Eleazar V. Raneses 1 ◽  
Bennidict P. Pueyo 1

Geophysical changes of the river outlets, riverbanks and coastlines in Alaminos, Pangasinan were measured using Google Earth from 2009 to 2014. On the other hand, actual measurements were gathered using South Total Station (NTS-362R6L) in 2015. The insights of the residents regarding feature changes of the river were obtained through one on one interview. Root Mean Square Errors (RMSE) were computed for measurement and horizontal positional accuracy of Google Earth. To perceive the effects of sea levels, historical data (2004-2015) from Bolinao, Philippines Tide Chart at online tides and currents predictions were also analyzed. Alaminos river outlets decreased in width size due to natural factor and human activities. Alaminos riverbank increased in width size which could be possibly due to natural calamities and weak bank resistance brought about by the frequent flooding caused by heavy rains and the emergency released of water from San Roque Dam. Generally the north and south coasts of Alaminos River increased and expanded. Rise in sea level is also a probable cause of changes wherein heights of low tides in Pangasinan Gulf is increasing overtime. The computed RMSE was low which indicate positional accuracy and measurement of Google Earth in the study area.

2007 ◽  
Vol 29 (3) ◽  
pp. 415-426
Author(s):  
Pham Van Ninh ◽  
Phan Ngoc Vinh ◽  
Nguyen Manh Hung ◽  
Dinh Van Manh

Overall the evolution process of the Red River Delta based on the maps and historical data resulted in a fact that before the 20th century all the Nam Dinh coastline was attributed to accumulation. Then started the erosion process at Xuan Thuydistrict and from the period of 1935 - 1965 the most severe erosion was contributed in the stretch from Ha Lan to Hai Trieu, 1965 - 1990 in Hai Chinh - Hai Hoa, 1990 - 2005 in the middle part of Hai Chinh - Hai Thinh (Hai Hau district). The adjoining stretches were suffered from not severe erosion. At the same time, the Ba Lat mouth is advanced to the sea and to the North and South direction by the time with a very high rate.The first task of the mathematical modeling of coastal line evolution of Hai Hau is to evaluate this important historical marked periods e. g. to model the coastal line at the periods before 1900, 1935 - 1965; 1965 - 1990; 1990 - 2005. The tasks is very complicated and time and working labors consuming.In the paper, the primarily results of the above mentioned simulations (as waves, currents, sediments transports and bottom - coastal lines evolution) has been shown. Based on the obtained results, there is a strong correlation between the protrusion magnitude and the southward moving of the erosion areas.


1991 ◽  
Vol 105 (1) ◽  
pp. 1-31
Author(s):  
Saskia De Bodt

AbstractThe article starts by taking stock of research into North and South Netherlandish professional embroidery in the sixteenth and seventeenth centuries. Such embroidery, which was rarely or never signed, and much of which has been lost, has hitherto been studied largely on stylistic grounds and grouped around noted schools of painting. Classifications include 'circle of Jacob Cornelisz van Oostsanen', for instance, or 'Leiden school/influence of Lucas van Leyden'. The author advocates a more relative approach to such classification into schools. She suggests that only systematic archive research in each location can shed new light on the production of embroidery studios and that well-founded attributions hinge solely on such research. The embroidery produced in Utrecht between 1500 and 1580 is cited as an example. The invoices of Utrecht parish and collegiate churches from circa 1500 to the Reformation record not onlv commissions to painters, goldsmiths and sculptors but also many items referring to textiles, notably embroidery. Together they provide a clear and relatively complete picture of the activities of sixteenth-century Utrecht embroiderers, whose principal customers were the churches. The items in question moreover exemplify the craft of the North Netherlandish embroiderer in that period in general in terms of what was produced as well as of the method and position of these artistic craftsmen, who were less overshadowed by painters than is generally assumed. A brief introduction outlining the organization of professional Utrecht embroiderers, who became independent of the tailors' guild in 1610 and acquired their own warrant, is followed by the analysis of an order from the Buurkerk in Utrecht for crimson paraments in 1530: three copes, a chasuble and two dalmatics. The activities of all those involved in their production are recorded : the merchants who supplied the fabric, the tracers of the embroidery patterns, the embroiderer, the cutter, various silver-smiths and the maker of the chest in which the set of garments was kept. The embroiderer was the best-paid of all these specialists. It is interesting to note that some Utrecht guild-members worked free of charge on these paraments, and that the collection at the first mass at which they were worn was very generous. There were probably political reasons for this: some of the donators, Evert Zoudenbalch and Goerd van Voirde, had been mayors at the time of the guild rebellion in Utrecht, and the Buurkerk was the parish church where the guild altars stood. After this detailed example the author discusses Utrecht embroiderers known by name and their studios,comparing them with a list of major commissions carried out for churches in Utrecht (appendix I). It transpires that in each case one studio received the most important Utrecht orders. This is followed by the reconstruction of three leading figures' careers. First Jacob van Malborch, active till 1525; a contract (1510) with the Pieterskerk in Utrecht regarding blue velvet copes is cited (appendix 11). He is followed by the embroiderers Reyer Jacobs and Sebastiaen dc Laet. Among his other activities, the latter was responsible for repairing and altering the famous garments of Bishop David of Burgundy. Items on invoices arc then cited as evidence that the sleeves of two dalmatics now in the Catharijneconvent Museum, embroidered on both sides with aurifriezes donated by Bishop David, were made by Jacob van Malborch in 1504/1505. This shows that systematic scrutiny of invoices and the results of archive research concentrated on individual embroiderers in a single city, compared with preserved items of embroidery, yield information that can lead to exact attributions to an artist or a studio (figs.4a to c and 5a to c). The Catharijneconvent Museum also possesses a series of figures of saints embroidered by the same hand (fig. 14). Finally, the author points out that a group of embroidered work (previously mentioned by H. L. M. Defoer in the catalogue Schilderen met gouddraad en zyde (1987)) which historical data suggest was done in Utrecht and which was produced in the same period, are almost certain to have come from Jacob van Malborch's studio, despite the lack of archival evidence (figs. 6 to 13).


Radiocarbon ◽  
2004 ◽  
Vol 46 (2) ◽  
pp. 517-529 ◽  
Author(s):  
Michael K Stewart ◽  
Joseph T Thomas ◽  
Margaret Norris ◽  
Vanessa Trompetter

Radiocarbon, 18O, and chemical concentrations have been used to identify groundwater recharged during the last ice age near Nelson, New Zealand. Moutere Gravel underlies most of the Moutere Depression, a 30-km-wide system of valleys filled with Plio-Pleistocene gravel. The depression extends northwards into Tasman Bay, which was above sea level when the North and South Islands of New Zealand were connected during the last glaciation. The aquifers are tapped by bores up to 500 m deep. Shallow bores (50–100 m) tap “pre-industrial” Holocene water (termed the “modern” component) with 14C concentrations of 90 ± 10 percent modern carbon (pMC) and δ18O values of −6.8 ± 0.4, as expected for present-day precipitation. Deeper bores discharge water with lower 14C concentrations and more negative 18O values resulting from input of much older water from depth. The deep end-member of the mixing trend is identified as paleowater (termed the “glacial” component) with 14C concentration close to 0 pMC and more negative 18O values (-7.6). Mixing of the modern and glacial components gives rise to the variations observed in the 14C, 18O, and chemical concentrations of the waters. Identification of the deep groundwater as glacial water suggests that there may be a large body of such water onshore and offshore at deep levels. More generally, the influence of changing sea levels in the recent past (geologically speaking) on the disposition of groundwaters in coastal areas of New Zealand may have been far greater than we have previously realized.


2019 ◽  
Vol 69 (Supplement_6) ◽  
pp. S474-S482
Author(s):  
Stephen Baker ◽  
Mohammad Ali ◽  
Jessica Fung Deerin ◽  
Muna Ahmed Eltayeb ◽  
Ligia Maria Cruz Espinoza ◽  
...  

Abstract Background Robust household sampling, commonly applied for population-based investigations, requires sampling frames or household lists to minimize selection bias. We have applied Google Earth Pro satellite imagery to constitute structure-based sampling frames at sites in Pikine, Senegal; Pietermaritzburg, South Africa; and Wad-Medani, Sudan. Here we present our experiences in using this approach and findings from assessing its applicability by determining positional accuracy. Methods Printouts of satellite imagery combined with Global Positioning System receivers were used to locate and to verify the locations of sample structures (simple random selection; weighted-stratified sampling). Positional accuracy was assessed by study site and administrative subareas by calculating normalized distances (meters) between coordinates taken from the sampling frame and on the ground using receivers. A higher accuracy in conjunction with smaller distances was assumed. Kruskal-Wallis and Dunn multiple pairwise comparisons were performed to evaluate positional accuracy by setting and by individual surveyor in Pietermaritzburg. Results The median normalized distances and interquartile ranges were 0.05 and 0.03–0.08 in Pikine, 0.09 and 0.05–0.19 in Pietermaritzburg, and 0.05 and 0.00–0.10 in Wad-Medani, respectively. Root mean square errors were 0.08 in Pikine, 0.42 in Pietermaritzburg, and 0.17 in Wad-Medani. Kruskal-Wallis and Dunn comparisons indicated significant differences by low- and high-density setting and interviewers who performed the presented approach with high accuracy compared to interviewers with poor accuracy. Conclusions The geospatial approach presented minimizes systematic errors and increases robustness and representativeness of a sample. However, the findings imply that this approach may not be applicable at all sites and settings; its success also depends on skills of surveyors working with aerial data. Methodological modifications are required, especially for resource-challenged sites that may be affected by constraints in data availability and area size.


2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Chenlu Huang ◽  
Qinke Yang ◽  
Yuhan Guo ◽  
Yongqiang Zhang ◽  
Linan Guo

AbstractThe Qin Mountains region is one of the most important climatic boundaries that divide the North and South of China. This study investigates vegetation covers changes across the Qin Mountains region over the past three decades based on the Landsat-derived Normalized Difference Vegetation Index (NDVI), which were extracted from the Google Earth Engine (GEE). Our results show that the NDVI across the Qin Mountains have increased from 0.624 to 0.776 with annual change rates of 0.0053/a over the past 32 years. Besides, its abrupt point occurred in 2006 and the change rates after this point increased by 0.0094/a (R2 = 0.8159, p < 0.01) (2006–2018), which is higher than that in 1987–1999 and 1999–2006. The mean NDVI have changed in different elevation ranges. The NDVI in the areas below 3300 m increased, such increased is especially most obviously in the cropland. Most of the forest and grassland locate above 3300 m with higher increased rate. Before 2006, the temperature and reference evapotranspiration (PET) were the important driven factors of NDVI change below 3300 m. After afforestation, human activities become important factors that influenced NDVI changes in the low elevation area, but hydro-climatic factors still play an important role in NDVI increase in the higher elevations area.


2017 ◽  
Vol 43 (2) ◽  
pp. 56-65 ◽  
Author(s):  
Mohammad Ali GOUDARZI ◽  
René Jr. LANDRY

The horizontal positional accuracy of Google Earth is assessed in the city of Montreal, Canada, using the precise coordinates of ten GPS points spatially distributed all over the city. The results show that the positional accuracy varies in the study area between ∼0.1 m in the south to ∼2.7 m in the north. Furthermore, two methods are developed for correcting the observed positional errors: (a) using a set of transformation parameters between true coordinates of the geodetic points and their coordinates in Google Earth, and by (b) interpolating the misfit vectors at the geodetic points. The former method reduces the overall accuracy to ∼67 cm RMSE, whereas the latter one practically removes all the distortion (RMSE = 1 cm). Both methods can be developed for other places in the world subject to availability of appropriate control points. In addition, a displacement problem caused by the topography of the area and the viewing angle of the imaging satellite is discussed, and it is shown that the true positions can be shifted even up to several meters, as a consequence.


Sign in / Sign up

Export Citation Format

Share Document