Strona glówna
•
FAQ
•
Szukaj
•
Użytkownicy
•
Grupy
•
Galerie
•
Rejestracja
•
Profil
•
Zaloguj się, by sprawdzić wiadomości
•
Zaloguj
Forum Forum MESA !! Strona Główna
->
Wyniki
Napisz odpowiedź
Użytkownik
Temat
Treść wiadomości
Emotikony
Więcej Ikon
Kolor:
Domyślny
Ciemnoczerwony
Czerwony
Pomarańćzowy
Brązowy
Żółty
Zielony
Oliwkowy
Błękitny
Niebieski
Ciemnoniebieski
Purpurowy
Fioletowy
Biały
Czarny
Rozmiar:
Minimalny
Mały
Normalny
Duży
Ogromny
Zamknij Tagi
Opcje
HTML:
TAK
BBCode
:
TAK
Uśmieszki:
TAK
Wyłącz HTML w tym poście
Wyłącz BBCode w tym poście
Wyłącz Uśmieszki w tym poście
Kod potwierdzający: *
Wszystkie czasy w strefie EET (Europa)
Skocz do:
Wybierz forum
Nabór do ZESPÓŁ Forum MESA
----------------
Nabór
MESA - DRUŻYNY
----------------
GKS Bełchatów
Cracovia Kraków
Dyskobolia Grodzisk Wielkopolski
Górnik Zabrze
Jagiellonia Białystok
Korona Kielce
Lech Poznań
Legia Warszawa
ŁKS Łódź
Odra Wodzisław Śląski
Polonia Bytom
Ruch Chorzów
Wisła Kraków
Zagłębie Lubin
Zagłębie Sosnowiec
MESA - OGÓLNIE
----------------
Regulamin
Terminarz
Sędziowie
Wyniki
DLA KIBICA
----------------
Typer
Rozrywka
Sonda
INNE
----------------
Hydepark
Reklama
PARTNERZY
----------------
Parnerzy w reklamie i realizacji projektu !!
Przegląd tematu
Autor
Wiadomość
ncycgdxhl
Wysłany: Nie 21:04, 20 Lut 2011
Temat postu: East Asian Winter Monsoon and the relationship bet
East Asian Winter Monsoon and the relationship between drought and flood in Huaihe River Basin in summer
Weather dependents ∞ 1997 No. 6 in January cut the tropical western Pacific Figure 6 Xi Xi high latitude anomalies compliance practice {dagger month change in the solid line for the flood. Dotted line for the early years; vertical axis for the month, the abscissa is willing not only in the line of latitude anomaly intensity long wave trough and ridge, and but also in the subtropical ridge on the strength or position changes from winter to summer anomalies toward their the opposite direction. 3 Summary and discussion of the East Asian winter monsoon circulation changes in the world a very important part, it has significant interannual variations. It's unusual for the late circulation and weather will inevitably have an impact. We explore the Huaihe River Basin from the summer drought and flood forecasting into projects and starting to study the early stage of their differences in large-scale circulation features,
timberland boots
, as well as the relationship between winter and summer circulation. The main conclusion is: 3.1 early summer flood of Huaihe River before the winter weather can be found in its obvious sign. For the earlier years of winter,
belstaff milano
, its large scale circulation features are: the radial-degree circulation in Europe and Asia, East Asia and stronger than normal trough extending southwards, Eurasia and the E g of the thumb region Huo spinach strong ridge of high pressure, Acute high-altitude Tibetan strong and expanded to the west end of Asian winter monsoon is strong cold wave activities between the Central Tibetan situation; and winter floods years ago, the circulation is relatively flat, weak and North East Asia trough shrink, cold wave activity is weak, Asia cold high on the mainland are also weak. 3.2 The circulation characteristics of the tropics is different: For the early years, due to strong cold surge events,
ghd piastre
, the Asian continent along the thumb of the northerly wind is stronger than the year round,
ghd outlet
, it makes 105 ~ E at the cross-equatorial flow to strong, the western Pacific warm pool area of the vapor activity much stronger than normal. Cover is bound to strong local ey circulation puppets; and the characteristics of winter floods years ago, the opposite. Since we are using the season average and more than one example of the homes into, so in time and space above reflects the difference between large-scale circulation features. Significant difference of 3.3 years of drought and flood is also reflected in the seasonal transition from summer on the winter solstice. Early in summer, winter and spring circulation started by the previous degree of strong radial evolution toward the zonal circulation, to May,
ugg stiefel
, the situation is completely similar to the summer drought; and floods and vice versa. Subtropical high ridge line position and intensity of seasonal evolution of the trend is opposite. 3.4 these results are given in winter and summer circulation and weather links between the evidence. Winter Monsoon is a very strong signal, it not only affects the flow patterns of atmospheric circulation at that time, and continues to affect the underlying surface conditions and post-circulation and weather. These results also with the foreign long-term drought forecast for the summer to provide effective physical basis.
fora.pl
- załóż własne forum dyskusyjne za darmo
Theme
FrayCan
created by
spleen
&
Download
Powered by
phpBB
© 2001, 2005 phpBB Group
Regulamin