Sentences with phrase «ice anomalies»

The effects of North Atlantic SST and sea ice anomalies on the winter circulation in CCM3.

But a look at the plotted sea ice anomaly data we -LSB-...]

The chart below is from the Cryosphere Today and shows the sea ice anomaly for the short period of time (since 1979) we have been able to observe it by satellite.

1 (kim) Watch the Argos bouys for dropping sea temperatures, the RSS and UAH satellite thermometers for cooling tropospheric temperatures, Bob B's links for sea level dropping, and cryosphere for polar ice anomalies.

The key issue is that since last year's dramatic summer ice anomaly, the winter ice that formed in that newly opened water is relatively thin (around 1 meter), compared to multi-year ice (3 meters or so).

Sea ice anomalies at the springtime maximum probably have more to do with what is happening to weather over subarctic seas rather than what is happening to preconditioning of sea ice in the Arctic Basin proper.

Magnusdottir, G., R. Saravanan and C. Deser, 2003: The modelled response of the atmospheric winter circulation to North Atlantic SST and sea - ice anomalies corresponding to multidecadal trends.

Under these conditions, younger, thinner ice anomalies recirculate back to the Alaskan coast more quickly, decreasing the time that new ice has to ridge and thicken before returning for another melt season.

Balmaseda, M. A., Ferranti, L., Moteni, F. & Palmer, T. N. Impact of 2007 and 2008 Arctic ice anomalies on the atmospheric circulation: implications for long - range predictions.

Sea ice anomaly chart on Cryosphere Today seems to be stuck at the bottom -2.5 km2, which is quite expected given the roundness of the remaining pack.

But a look at the plotted sea ice anomaly data we see that sea ice has in fact stabilized over the past 11 years.

«Our future studies will look to compare the role of the AMO compared to Arctic sea ice anomalies, which have also been shown to affect atmospheric circulation patterns and promote colder, more extreme winters.»

Alexander, M.A., et al., 2004: The atmospheric response to realistic Arctic sea ice anomalies in an AGCM during winter.

Global sea ice anomaly is positive: Physicist: «Imagine that.

Linkages between Arctic summer circulation regimes and regional sea ice anomalies.

Deser, C, G. Magnusdottir, R. Saravanan and A. Philips, 2004: The effects of the North Atlantic SST and sea - ice anomalies on the winter circulation in CCM3.

Some processes arise through interactions with other parts of the climate system such as the ocean (for example as manifested through sea surface temperature anomalies), sea ice anomalies, snow cover anomalies as well as through coupling to the circulation in the stratosphere.

G. Magnusdottir, C. Deser and R. Saravanan, 2004: The effects of North Atlantic SST and sea - ice anomalies on the winter circulation in CCM3.