Multiplication d'un Nombre à 3 Chiffres par un Nombre à 3 Chiffres (Gros Caractère) avec une Espace comme Séparateur de Milliers (A)

The linear response to such is forc- ing is again periodic and the temperature regression can be shown to increase for increasing forcing periods, reaching an equilibrium level

These dates require deglaciation before this time, and a maximum glacial ELA lowering of <500 m, far less than the purported global average of ∼1000 m for the LGM (Broecker

vegetation changes also occurred in the Kathmandu Valley: the odd-numbered zones of the RB core most likely cor- respond to glacial periods when C 4 plants

Considered processes depict changes in SST (SST), sea level (SEAL), sea ice (SICE), NADW formation (NADW), Southern Ocean vertical mixing (SOX), iron fertilisation in Southern

Another method to unravel the climate changes from geothermal data is based on the joint processing of surface air temperature (SAT) recorded at meteorological observatories

Using a combination of proxy records and results of a three dimensional climate model, we show that European summer temperatures roughly a millennium ago were compa- rable to those

In our situation, the approach to calibrate the ST UHF radar must be different and the method consists of using the re- flectivity computed from the drop-size distribution

We present high- time resolution data from SuperDARN HF radars in both the Northern and Southern Hemispheres which describe the high-latitude ionospheric response in the cusp region