The Lower Depths

change in the ocean depth. There are three distinctive zones that can be classified along the depth which is the Epipelagic which extends from the sea surface to a depth of 200 meters, the mesopelagic which extends from a depth of 200 meters to a depth of a 1000 meters and then the Deep sea which extends from a depth of a 1000 meters to the sea floor (Castro & Huber, 2010). The Deep sea can then be divided into a further three zones (Figure 01) Bathypelagic which extends from a depth of a 1000 meters

Discussion The results of the regression test comparing dissolved carbon dioxide in parts per million with salinity in parts per thousand at depth show that there is a correlation between the data as they have a p value less than 0.01 (Figure 8). Comparatively, the results of the regression test comparing dissolved carbon dioxide in parts per million with salinity in parts per thousand at the surface show that there is a correlation between the data as they have a p value less than 0.01 (Table 9)

palm trees placed lower on the page. Not only does the artist use diminution of scale, but they also use vertical location. The bushier palm trees n the back left side of the composition all appear to be the same size, but because some are placed higher on the page, they appear to be further away than the ones placed lower on the page. The artist use of overlapping helps achieve perception of depth. By overlapping the trees it makes it look like the painting has much more depth. Because of all of

format, compression techniques image resolution and colour depth have on file size and image quality. In this report, I will talk about my understanding of the impact in various file format, the different compression techniques, and different resolutions and different colour depth. I will show print screens of different types of compression techniques, megapixels under image quality & resolution and three different types of colour depths. I will explain the reasons why some are larger compared to

Impact that file format, compression techniques, image resolution and colour depth have on file size and image quality - D2 In this report I will be discussing the different file formats, compression techniques, image resolution and colour depth. I will be explaining the different purposes, then, after I have issued an in-depth explanation of image quality and file size I will be completing a final conclusion about the best ones to use for certain tasks. Seen as there are numerous different uses

with the change in the ocean depth. There is three distinctive zones that can be classified the Epipelagic which extends from the sea surface to a depth of 200 meters, the mesopelagic which extends from a depth of 200 meters to a depth of a 1000 meters and then the Deep sea which extends from a depth of a 1000 meters to the sea floor (Castro & Huber, 2010). The Deep sea can then be divided into a further three zones (Figure 01) Bathypelagic which extends from a depth of a 1000 meters to 4000 meters

Theoretical y2 = 0.0262m Measured y2 = 0.0280±0.001m Energy discrepancy = 0.0443J Based on the hydraulic theory velocity=discharge / height, with the same discharge, lower height of stream flows with higher velocity than stream with greater height. The energy equation K.E.=mv22 and E=y+v22g also show Measured y2 contains lower

In this lab the researchers were testing how different massed “meteorites” dropped at the same distance affect the depth of an impact crater. The researchers predicted that if the mass of the object in the egg increases than the depth of the impact crater will also increase because gravity will pull down harder on the heavier object than it will the lighter object. The hypothesis was supported because the greater the mass of an object than the deeper the impact crater will be because the greater

impact on the snow industry economy. General Effects Climate change causes increases in temperature, evaporation, extreme rainfall events and solar radiation along with a decrease in snow fall. This impacts the length of the snow season and the depth and coverage of snow. There is an

maximum metal uptake capacity (qcal) under different process conditions and were compared with the experimental values (qexp) in relation to the estimated values of ka and No. As shown in Table 1a and b, the values ka decreased with increasing bed depth and influent metal concentration, but increase with increasing flow rates. Meanwhile, the values of No declined with the increase in bed height and flow rate. This trend can be explained on the fact that at increased bed heights more number of active