86 research outputs found
Π Π°Π·Π²ΠΈΡΠΈΠ΅ ΠΊΡΠ΅Π΄ΠΈΡΠ½ΠΎΠ³ΠΎ ΡΡΠ½ΠΊΠ° Π£ΠΊΡΠ°ΠΈΠ½Ρ ΠΈ ΠΡΡΠΌΠ°
Π Π΄Π°Π½Π½ΠΎΠΉ ΡΡΠ°ΡΡΠ΅ ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½ ΡΡΠ°Π²Π½ΠΈΡΠ΅Π»ΡΠ½ΡΠΉ Π°Π½Π°Π»ΠΈΠ· ΠΏΡΠ΅Π΄ΠΎΡΡΠ°Π²Π»Π΅Π½ΠΈΡ ΠΊΡΠ΅Π΄ΠΈΡΠ½ΡΡ
ΡΠ΅ΡΡΡΡΠΎΠ² ΡΠΊΡΠ°ΠΈΠ½ΡΠΊΠΈΠΌΠΈ Π±Π°Π½ΠΊΠ°ΠΌΠΈ ΠΈ Π±Π°Π½ΠΊΠ°ΠΌΠΈ ΠΠ Π Π·Π° 2000-2006Π³Π³. ΠΠ΅ΡΠ°Π»ΡΠ½ΠΎ ΡΠ°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°ΡΡΡΡ ΠΊΡΠ΅Π΄ΠΈΡΡ, ΠΏΡΠ΅Π΄ΠΎΡΡΠ°Π²Π»Π΅Π½Π½ΡΠ΅ Π² ΡΠΊΠΎΠ½ΠΎΠΌΠΈΠΊΡ Π£ΠΊΡΠ°ΠΈΠ½Ρ ΠΈ ΠΡΡΠΌΠ°, ΠΏΠΎ ΡΡΠΎΠΊΠ°ΠΌ ΠΈ ΠΏΠΎ ΡΠ΅Π»Π΅Π²ΠΎΠΌΡ Π½Π°Π·Π½Π°ΡΠ΅Π½ΠΈΡ.Π£ Π΄Π°Π½ΡΠΉ ΡΡΠ°ΡΡΡ ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½ΠΈΠΉ ΠΏΠΎΡΡΠ²Π½ΡΠ»ΡΠ½ΠΈΠΉ Π°Π½Π°Π»ΡΠ· Π½Π°Π΄Π°Π½Π½Ρ ΠΊΡΠ΅Π΄ΠΈΡΠ½ΠΈΡ
ΡΠ΅ΡΡΡΡΡΠ² ΡΠΊΡΠ°ΡΠ½ΡΡΠΊΠΈΠΌΠΈ Π±Π°Π½ΠΊΠ°ΠΌΠΈ Ρ Π±Π°Π½ΠΊΠ°ΠΌΠΈ ΠΠ Π Π·Π° 2000-2006Π³Π³. ΠΠ΅ΡΠ°Π»ΡΠ½ΠΎ ΡΠΎΠ·Π³Π»ΡΠ΄Π°ΡΡΡΡΡ ΠΊΡΠ΅Π΄ΠΈΡΠΈ, Π½Π°Π΄Π°Π½Ρ Π² Π΅ΠΊΠΎΠ½ΠΎΠΌΡΠΊΡ Π£ΠΊΡΠ°ΡΠ½ΠΈ Ρ ΠΡΠΈΠΌΡ, ΠΏΠΎ ΡΠ΅ΡΠΌΡΠ½Π°Ρ
Ρ Π·Π° ΡΡΠ»ΡΠΎΠ²ΠΈΠΌ ΠΏΡΠΈΠ·Π½Π°ΡΠ΅Π½Π½ΡΠΌ.In given article the analysis of the credit market in Ukraine and in Crimea is shown. The main idea of the article this consideration of the credits on kinds and on a special-purpose designation
Comparison of climate change signals in CMIP3 and CMIP5 multi-model ensembles and implications for Central Asian glaciers
Climate Changes and Their Elevational Patterns in the Mountains of the World
Quantifying rates of climate change in mountain regions is of considerable interest, not least because mountains are viewed as climate βhotspotsβ where change can anticipate or amplify what is occurring elsewhere. Accelerating mountain climate change has extensive environmental impacts, including depletion of snow/ice reserves, critical for the world's water supply. Whilst the concept of elevation-dependent warming (EDW), whereby warming rates are stratified by elevation, is widely accepted, no consistent EDW profile at the global scale has been identified. Past assessments have also neglected elevation-dependent changes in precipitation. In this comprehensive analysis, both in situ station temperature and precipitation data from mountain regions, and global gridded data sets (observations, reanalyses, and model hindcasts) are employed to examine the elevation dependency of temperature and precipitation changes since 1900. In situ observations in paired studies (using adjacent stations) show a tendency toward enhanced warming at higher elevations. However, when all mountain/lowland studies are pooled into two groups, no systematic difference in high versus low elevation group warming rates is found. Precipitation changes based on station data are inconsistent with no systematic contrast between mountain and lowland precipitation trends. Gridded data sets (CRU, GISTEMP, GPCC, ERA5, and CMIP5) show increased warming rates at higher elevations in some regions, but on a global scale there is no universal amplification of warming in mountains. Increases in mountain precipitation are weaker than for low elevations worldwide, meaning reduced elevation-dependency of precipitation, especially in midlatitudes. Agreement on elevation-dependent changes between gridded data sets is weak for temperature but stronger for precipitation
Distributed fiber optic shape sensing along shotcrete tunnel linings: Methodology, field applications, and monitoring results
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