But make sure to check again because sometimes the game does not place it according to their perfect positions. You can tap the auto-fill button if you are lazy to do this. For example - SG type should be placed in the SG slot. If you deploy the players on their perfect position in the deck or during the battle preparations, the game will provide a boost to all the stats.Īll you have to do is drag and drop the cards to their perfect position. In the next part, you will learn about the positions. And, select the one who has the best Defense stat. Suppose, the match or round type is defense, then you have to pay attention to the defense stat of each player. On your screen, the game will show you the round or match type Defense, Offense, Rebounding, Playmaking, etc. Now, during the card battle, you have to choose the right player - depends on the match type. When it comes to the cards info, you should know about the cards rarity, abilities, how the ability mechanics work, card position, etc. Current Conditions.Last Updated on August 22, It also lets you connect to the console accounts for the latest features such as Face Scan, Locker code. Allows cold, Arctic air to be transported south and increases the likelihood of interaction between the northern and southern jet streams Jet stream interaction often result in a combining of energy phasingwhich leads to rapid, intense surface cyclogenesis over the southern U. Positional Effects of the NAO Favorable positioning of the geopotential height anomalies within the negative phase of the NAO appears to enhance snowfall potential in the eastern U.Ītmospheric features in a "wet-based" negative NAO disrput the polar jet stream, causing it to buckle and move southward into the Southeast. The decrease in the westerlies allows cold air to build up over Canada, and this combined with below average heights troughing over the eastern U.īelow average geopotential heights are often observed over the eastern U. This decreased pressure gradient results in a slackening of the westerlies. Above average geopotential heights are observed over the eastern U. The increased westerlies allow cold air to drain off the North American continent rather than letting it build up and move south. This strengthening results in an increased pressure gradient over the North Atlantic, which cause the westerlies to increase in strength. It is also important to note that the AO and NAO are two separate indices that are ultimately describing the same phenomenon of varying pressure gradients in the northern latitudes and the resultant effects on temperature and storm tracks across the continent. Fluctuations in the strength of these features significantly alters the alignment of the jet stream, especially over the eastern U.
It is important to note that these two locations are most commonly used to measure the NAO, but studies have found that the pressure centers move around on a seasonal basis, and other locations have also been used for measuring this index. The opposite is true when the AO is positive: the polar circulation is stronger which forces cold air and storms to remain farther north. The result of the weaker westerlies is that cold, Arctic air is able to push farther south into the U. In the negative phase, the polar low pressure system also known as the polar vortex over the Arctic is weaker, which results in weaker upper level winds the westerlies. It consists of a positive phase, featuring below average geopotential heightswhich are also referred to as negative geopotential height anomaliesand a negative phase in which the opposite is true. This results in a phenomenon referred to as high latitude blocking, which allows cold air to drain from Alaska and Canada into the U. When the Icelandic low and Azores high are weaker, above average mb heights are located near Iceland, and below average heights near the Azores Islands. In turn, above normal temperatures are seen over the eastern U. A stronger Icelandic low and Azores high translates into lower than average mb heights near Iceland, and above average heights near the Azores Islands.