RSS-based localization considering topographical feature for pasturing

Author(s):  
K. Yokoo ◽  
T. Nishidoi ◽  
H. Urabe ◽  
T. Ikenouchi ◽  
T. Ninomiya ◽  
...  
The Auk ◽  
2019 ◽  
Vol 136 (3) ◽  
Author(s):  
David V Gesicki ◽  
Erica L Cech ◽  
Verner P Bingman

Abstract Migratory birds encounter the Great Lakes while moving through eastern North America toward breeding grounds to the North, which offers a good opportunity to study variation in migratory behavior as birds face a potentially influencing topographical feature. Using passive infrared technology, we documented the direction of relatively low-flying, nocturnal, mostly passerine migration in spring along the southern coast of Lake Erie’s western basin. We examined the extent to which spring migrants flew across Lake Erie as a continuation of the inland, northeasterly broad front migratory direction, as determined by weather radar and infrared observations, or displayed a tendency to deviate to more closely follow the direction of the coastline. We found that an estimated 62% of all low-flying migrants deviated their flight directions toward the coast of Lake Erie at 2 coastal sites, Cedar Point and Ottawa, which were characterized by northwest–southeast oriented coastlines. Migrants at a third coastal location, Maumee Bay, which has a more east–west oriented coastline, did not display similarly deviated flight directions. We found that even when winds were energetically favorable for a lake crossing, many migrants still routinely displayed deviated flight directions that approached paralleling the coastline. Further, the mean flight direction at one site, Ottawa, shifted more in the direction of the coastline as the night progressed, suggesting that time of night could influence the shift to a more coastal flight direction. The data indicate that the western basin of Lake Erie acts as a salient topographical feature influencing the flight directions of nocturnal migrants. The data further suggest that birds are making active decisions while in flight, based on current environmental and physiological conditions, about whether to continue to cross Lake Erie or take a coastal detour.


1978 ◽  
Vol 7 ◽  
pp. 61-93 ◽  
Author(s):  
D. W. Rollason

Secgan be þam Godes sanctum þe on Engla lande ærost reston is the title of a short document in Old English which is extant in two manuscripts, Cambridge, Corpus Christi College 201, pp. 149–51, and London, British Library, Stowe 944, 34v–39r. These manuscripts are dated to the middle and the first half of the eleventh century respectively on the evidence of their script. A third copy was once in London, British Library, Cotton Vitellius D. xvii but was destroyed in the fire of 1731. The only scholarly edition is that of Felix Liebermann. The document mentions the resting-places of eighty-nine saints: all but one of these places are in England and all but ten of the saints were active in England. The usual formula is of the type, ‘Ðonne resteð sanctus Congarus confessor on Cungresbirig’ (37b), but in many cases the place is further defined by reference to some topographical feature, most often a river, as, for example, ‘Ðonne resteð sanctus Iohannes biscop on þare stowe Beferlic, neah þare ea Hul’ (5a).


2011 ◽  
Vol 1 (8) ◽  
pp. 16 ◽  
Author(s):  
Masashi Hom-ma ◽  
Choule Sonu

Despite a number of valuable contributions by many predecessors, namely F. F. Shepard (Ref. 1) and Q. H. Keulegan (Ref. 2), our knowledge regarding the effect of a longshore bar on the sedimentary process of a coast has long remained a plausible, qualitative understanding that a longshore bar constitutes a zone of active migration of bottom deposit due to agitation of breakers and currents. This was probably due mainly to the difficulty of performing an accurate hydrographic survey near the breaker zone. On the other hand, the geometrical characteristics along a single bar profile, which was sounded off either from a stable pier (Ref. 1) or a suspended cable (Ref. 3) resulted in a hopeless scatter. An aerial photograph, if taken under favorable conditions, may show an Interesting picture of submerged topographies In a distinct contrast made by the bright tone of a shallow bar crest or a shoal, against the dark background of a deep trough or a rock bottom. By comparing such photographic records with convenient soundings derived from some of the Japanese coasts, an Interesting topographical feature of a longshore bar has been disclosed. A longshore bar may attain a rhythmic pattern consisting of echelons of arcuate (or lunate) bar unit, which in entire appearance strongly resembles that of a honeycomb. It has also been discovered that a rhythmic bar pattern is correlated with other Important factors either dynamic or static, which participate in the general processes of a coast, namely the shoreline configuration, the shoreface slope and deposit, the topographies on the offshore bottom, transformation of Incident waves, the longshore currents and the littoral drifts. The authors have further attempted to develop a hypothetical concept on the origin of littoral rhythms as well as the behaviors of alongshore movement of sediment, and to consider their engineering lmplications on the basis of such findings. Although our success which has been achieved so far is yet incomplete due to lack of available data, it is believed that the approach and concept as proposed in the present paper may suggest an encouraging line of research toward formulating a unified macroscopic view on the mechanics of the littoral process.


2017 ◽  
Author(s):  
Göran Björk ◽  
Martin Jakobsson ◽  
Karen Assmann ◽  
Leif Andersson ◽  
Johan Nilsson ◽  
...  

Abstract. The Lomonosov Ridge represents a major topographical feature in the Arctic Ocean which has a large effect on the water circulation and the distribution of water properties. This study presents detailed bathymetric survey data along with hydrographic data at two deep passages across the ridge: A southern passage (80–81° N) where the ridge crest meets the Siberian continental slope and a northern passage around 84.5° N. The southern channel is characterized by smooth and flat bathymetry around 1600–1700 m with a sill depth slightly shallower than 1700 m. A hydrographic section across the channel reveals an eastward flow with Amundsen Basin properties in the southern part and a westward flow of Makarov Basin properties in the northern part. The northern passage includes an approximately 72 km long and 33 km wide trough which forms an intra basin in the Lomonosov Ridge morphology (the Oden Trough). The eastern side of Oden Trough is enclosed by a narrow and steep ridge rising 500–600 m above a generally 1600 m deep trough bottom. The deepest passage (the sill) is 1470 m deep and located on this ridge. Hydrographic data show irregular temperature and salinity profiles indicating that water exchange occurs as midwater intrusions bringing water properties from each side of the ridge in well-defined but irregular layers. There is also morphological evidence that some rather energetic flows may occur in the vicinity of the sill. A well expressed deepening near the sill may be the result of seabed erosion by bottom currents.


1910 ◽  
Vol 7 (6) ◽  
pp. 244-258
Author(s):  
Alfred P. Young

In a previous paper it was shown that one prominent topographical feature of the Tarntal district, the great cirque called the ‘Grübl’,. could be explained as the effect of erosion by a short icetongue which formed when the snow-line persisted for a time at about 2400 metres above sea-level. The basin-shaped hollow of the Upper Tarntal was held to be due to another stand of the snow-limit at 2650 metres. It remains to be seen whether these conclusions are supported by evidence of a similar nature collected over a wider area.


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