Amazonian flood plains(passive) influenced byAmazonian flood plains

mild weather(passive) caused bymild weather

Rainfall variability in the tropical Pacific(passive) caused byRainfall variability in the tropical Pacific

2623 - 2635 Australian rainfall(passive) is strongly influenced by2623 - 2635 Australian rainfall

large scale climate variability(passive) caused bylarge scale climate variability

The most prominent signature in the global mean sea level interannual variability(passive) is caused byThe most prominent signature in the global mean sea level interannual variability

almost all the CS&GM coupled modes ... except the transition mode ... and that the North Atlantic Oscillation ( NAO ) in February has a strong negative correlation with the dipole and transition modesinfluencesalmost all the CS&GM coupled modes ... except the transition mode ... and that the North Atlantic Oscillation ( NAO ) in February has a strong negative correlation with the dipole and transition modes

on monthly NO3 load and concentration , stream flow and precipitation in the Little River Watershed , Tifton , GA ARSinfluenceson monthly NO3 load and concentration , stream flow and precipitation in the Little River Watershed , Tifton , GA ARS

the abundance and movements of a marine top predator in coastal waters 48influencesthe abundance and movements of a marine top predator in coastal waters 48

the climate of Floridainfluencesthe climate of Florida

The climate of the Philippines(passive) is highly influenced byThe climate of the Philippines

droughts and floods,[2causingdroughts and floods,[2

most of these short term temperature changes(passive) are caused bymost of these short term temperature changes

not only the summer monsoon , but also the winter monsoon over East Asiainfluencednot only the summer monsoon , but also the winter monsoon over East Asia

from large - scale ocean – atmosphere interaction in the tropical Pacificresultsfrom large - scale ocean – atmosphere interaction in the tropical Pacific

winter weather patternsinfluenceswinter weather patterns

destructive flooding ... and drought in the West Pacificcauseddestructive flooding ... and drought in the West Pacific

coral δ18O at Santo through local salinity changes associated with the position of the South Pacific Convergence Zone and the movement of Santo 's associated salinity frontinfluencescoral δ18O at Santo through local salinity changes associated with the position of the South Pacific Convergence Zone and the movement of Santo 's associated salinity front

the major portion of the drought variability(passive) is influenced bythe major portion of the drought variability

This erratic climate has been found(passive) to be influenced very strongly byThis erratic climate has been found

the Guyanese climate as wellinfluencesthe Guyanese climate as well

floods , droughts and the collapse of fisheries ... therefore forecasting of ENSO is an important task in climate researchescausesfloods , droughts and the collapse of fisheries ... therefore forecasting of ENSO is an important task in climate researches

11 Changes(passive) caused by11 Changes

the Pacific Northwestcan strongly influencethe Pacific Northwest

moisture variability(passive) caused bymoisture variability

important changes in global weather patternscausesimportant changes in global weather patterns

In East Africa too , the climate seems(passive) to be influenced byIn East Africa too , the climate seems

the 1976–1977 climate shift(passive) caused bythe 1976–1977 climate shift

frequent droughts(passive) to be greatly influenced byfrequent droughts

severe droughtstriggeredsevere droughts

cyclical droughts(passive) caused bycyclical droughts

the abundance and movements of a marine top predator in coastal waters - Murdoch Research Repository Sprogis , K.R. , Christiansen , F. , Wandres , M. and Bejder , L.influencesthe abundance and movements of a marine top predator in coastal waters - Murdoch Research Repository Sprogis , K.R. , Christiansen , F. , Wandres , M. and Bejder , L.

the abundance and movements of a marine top predator in coastal waters Christiansen , Fredrik , et al . ; Sprogis , Kate R. ; Wandres , Moritz ; Bejder , Larsinfluencesthe abundance and movements of a marine top predator in coastal waters Christiansen , Fredrik , et al . ; Sprogis , Kate R. ; Wandres , Moritz ; Bejder , Lars

the negative correlation in tropical cyclone formation in the East Pacific and North Atlantic basins(passive) caused bythe negative correlation in tropical cyclone formation in the East Pacific and North Atlantic basins

from changes in air temperature over the Pacific Oceanresultsfrom changes in air temperature over the Pacific Ocean

episodic warming ( El Niño ) and cooling ( La Niña ) of the tropical Pacific and affects global weather patterns via atmospheric teleconnectionscausesepisodic warming ( El Niño ) and cooling ( La Niña ) of the tropical Pacific and affects global weather patterns via atmospheric teleconnections

to widespread drought in some areas and widespread flooding in othersleadingto widespread drought in some areas and widespread flooding in others

temperature change(passive) created bytemperature change

The Southeast 's climate , especially winter and spring seasons(passive) is ... influenced byThe Southeast 's climate , especially winter and spring seasons

in droughts in the southwestern Pacific , India and Africaresultin droughts in the southwestern Pacific , India and Africa