The north atlantic gulf stream is thought to make a greatly change of Northwest’s Europe climate. Otherwise, the summer isn’t too hot. The remaining landscape is occupied by meadows and grasslands, and 17% by native oak and evergreen oak forests. Other ara that have northwest europe is north coast of Spain (Basque country, north of navarre, asturias and Cantabria) most of france (far away from mediterranean), Germany, Norway, the, Western Azore off the south of Portugal and Southern area of Sweden. Amplitude of daily and annual temperature is large. In other European cities, only three to five genera usually accounted for 50–70% of all street trees planted (Pauleit et al., 2002). Furthermore, T. × europaea dominated just two sites. The intensity of rainfall is high and more frequent than any other area in the world. Strong light supports algal growth, which benefits mobile epifauna that eat periphyton, but not sessile epifauna, which are often susceptible to being overgrown. Figure 6.9 shows a regime shift, known generally as the Russell cycle, that has taken place in the western English Channel. Oxygen levels can be low in tributaries receiving dairy sewage, and phosphorus concentrations are 10-fold higher than in the main river (Elosegui et al. For example, in Hong Kong, the top 10 dominant species are 56% of the population. On soft sediments, epifaunal densities tend to decline with increasing depth due to the reduction in food input from the sunlit surface waters, though densities can be locally high where detritus accumulates.
Vegetation type is dominant of moss and bush. The annual temperature is lower than other area that has hot summer and cold winter. The Agüera drains 145 km2 in the Cantabric region in north Spain, between the Basque Country and Cantabria. Very little rainfall and is happened in the summer. There are many cyclonal air movements and constantly changing air pressure. Diversity is lower in the palaeotropics (possibly due to historical aridity), and decreases at higher altitudes and latitudes, but epiphytes can still be important in temperate forests with oceanic climates. Because marine fish stocks occupy large expanses of ocean, satellite remote sensing is now being applied to examine those variations in ocean conditions that cause natural fluctuations in the distribution, abundance, and availability of commercial stocks. The last edge of polar pole is an area of ocean climate with long and cold winter (but is not so cold) also it has cool and short summer (the mean temperature of this zone is 10˚C. So, this climate can be changing if there is a change in Ocean environment such as global warming in ocean, ocean pollution, acidification of the ocean, effect of sea level rise and also ocean phenomena. In comparison, only about 4% of the identified trees are unsuitable for retrofitting of permeable pavements. Rainfall much fell on the front slope and fell slightly in the rainfall shadow area. Both elements of climate is very big influence on the surface of the earth and life on it. It is washed from sediment samples and can be quantified using digital image analysis. 1993). Generally the air temperature is between 20- 23 ° C. Even in some places, the average annual temperature reaches 30 ° C. The average of annual amplitude temperature is small. Ocean climate is a reflection of nearby ocean, when it’s already fall, winter and early spring, the polar jet system is most active and then the fogs, cloudy skies and light drizzle often appear frequently. This direction of polar jet stream makes a system of low pressure, storms and fronts.
2006). It is now clear that the role of the environment cannot be excluded from fisheries theories, and that oceanographic data may contribute useful and necessary information to create new management theories. Characteristic is found in the Arctic and Antarctic regions, the temperature is never more than 10 ° C, while the average temperature of the coldest month is less than – 3 ° C. Climate area E, is divided into 2 types of climate, namely: Ocean climate is a name of typical climate that is happened at west coast in higher middle latitudes of continent. As the dreasing distance of the inland area and mediterranean Sea, the ocean climate of Northwest Europe gradually change, from dry summer or Mediterranean climate of Southern Europe to subtropical. The precipitation in that area is low rainfall with accompanied with a moment taufan. Its characteristics are as follows: Season climate is also called muson. This situation has improved somewhat in the last few years.
The rainfall happened to the area of ocean climate throughout the majority of year.
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