Operation Problems of the Cold Condensate Pipeline in Heaving Soils and Arctic Climate

Author(s):  
Evgeniy Markov ◽  
Sergey Pulnikov ◽  
Yuri Sysoev
Keyword(s):  
Author(s):  
Mark C. Serreze ◽  
Roger G. Barry

Author(s):  
E. S. Bodrova ◽  
V. V. Dolgosheev ◽  
I. M. Kirpichnikova ◽  
D. V. Korobatov ◽  
A. S. Martyanov ◽  
...  

2018 ◽  
Author(s):  
William Daniels ◽  
◽  
Isla S. Castañeda ◽  
Jeffrey M. Salacup ◽  
Julie Brigham-Grette
Keyword(s):  

AMBIO ◽  
2012 ◽  
Vol 41 (1) ◽  
pp. 10-22 ◽  
Author(s):  
Timothy M. Lenton

2006 ◽  
Vol 63 (3) ◽  
pp. 401-420 ◽  
Author(s):  
Harald Yndestad

Abstract The Arctic Ocean is a substantial energy sink for the northern hemisphere. Fluctuations in its energy budget will have a major influence on the Arctic climate. The paper presents an analysis of the time-series for the polar position, the extent of Arctic ice, sea level at Hammerfest, Kola section sea temperature, Røst winter air temperature, and the NAO winter index as a way to identify a source of dominant cycles. The investigation uses wavelet transformation to identify the period and the phase in these Arctic time-series. System dynamics are identified by studying the phase relationship between the dominant cycles in all time-series. A harmonic spectrum from the 18.6-year lunar nodal cycle in the Arctic time-series has been identified. The cycles in this harmonic spectrum have a stationary period, but not stationary amplitude and phase. A sub-harmonic cycle of about 74 years may introduce a phase reversal of the 18.6-year cycle. The signal-to-noise ratio between the lunar nodal spectrum and other sources changes from 1.6 to 3.2. A lunar nodal cycle in all time-series indicates that there is a forced Arctic oscillating system controlled by the pull of gravity from the moon, a system that influences long-term fluctuations in the extent of Arctic ice. The phase relation between the identified cycles indicates a possible chain of events from lunar nodal gravity cycles, to long-term tides, polar motions, Arctic ice extent, the NAO winter index, weather, and climate.


2015 ◽  
Vol 125 ◽  
pp. 91-97 ◽  
Author(s):  
Francesco Muschitiello ◽  
Qiong Zhang ◽  
Hanna S. Sundqvist ◽  
Frazer J. Davies ◽  
Hans Renssen

2021 ◽  
Author(s):  
Rajka Juhrbandt ◽  
Suvarchal Cheedela ◽  
Nikolay Koldunov ◽  
Thomas Jung

<p>The recently completed Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) can serve as reference to evaluate current and future ocean state of the Arctic Ocean. With this premise, we perform a virtual MOSAiC expedition in historical and ssp370-scenario experiments in data generated by CMIP6 models.<br><br>The timespan covered ranges from preindustrial times (1851-1860) through present-day up to a 4K world (2091-2100). Early results using AWI-CM model, suggest that for scenario simulations a thinning of the colder surface layer and a warming of the layer between 200 and 1200 m along the MOSAiC path can be expected, while there is no significant change in temperature below this depth. Results from other models will be presented.<br><br>The Python-centric tool used for the analysis simplifies preprocessing of a pool of CMIP6 data and selecting data on space-time trajectory. It exposes an interface that is agnostic to underlying model or its grid type. Code snippets are presented along to demonstrate the tool's ease of use with a hope to inspire such virtual field campaigns using other past observations or arbitrary trajectories.</p>


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