FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4385956449> ?p ?o ?g. }

• W4385956449 endingPage "230" @default.
• W4385956449 startingPage "207" @default.
• W4385956449 abstract "Global climate models are used to predict anthropogenic climate change and to plan social and economic activities under changing climatic conditions. At the same time, there are discrepancies between model projections and observed climate changes, especially in low latitudes and polar regions. One reason for the discrepancy may be insufficient attention to natural forcings on the climate system. Therefore, studies of the role of natural factors in the development of modern warming are relevant for&#x0D; improving the reliability of forecasts for the development of the climatic situation on Earth. Particular attention is paid to the impact of climate change in low latitudes on the Arctic. A significant contribution to these changes can be made by a long-term increase in low-latitude insolation. Most of the low latitudes&#x0D; are occupied by the ocean, which absorbs the bulk of the incoming solar radiation. The contribution of the increase in insolation to the increase in ocean surface temperature at low latitudes is estimated from the available data on insolation of the upper boundary of the atmosphere. The changes in SST at low latitudes are compared according to reanalysis data and calculations of global climate models. Comparison of climate changes in low latitudes and in the Arctic is made. The influence from low latitudes on the reduction in the area of sea ice and the increase in water temperature in the Arctic basin is estimated. Changes in the characteristics of the atmosphere and ocean at low latitudes, associated with an increase in insolation, after&#x0D; 3 years are manifested in changes in the characteristics of the climate and sea ice in the Arctic. This indicates the potential for improved global modeling of warming in the Arctic and at low latitudes when taking into account slow changes in radiative forcing at the upper boundary of the atmosphere due to the Earth’s orbital dynamics. Insolation trends at low latitudes are maximum in spring, i.e., in the vicinity of the vernal equinox in the Earth’s orbit. This indicates the influence of precession — a slow shift of the equinox point, when the influx of solar radiation to low latitudes is maximum, to the perihelion, where it will be 3 W/m2more." @default.
• W4385956449 created "2023-08-18" @default.
• W4385956449 creator A5067988774 @default.
• W4385956449 date "2023-07-11" @default.
• W4385956449 modified "2023-10-14" @default.
• W4385956449 title "Arctic climate warming: discrepancies between global climate&#x0D; models and observations and possible causes" @default.
• W4385956449 cites W1839424995 @default.
• W4385956449 cites W1951290059 @default.
• W4385956449 cites W1977466915 @default.
• W4385956449 cites W1983163307 @default.
• W4385956449 cites W1984514794 @default.
• W4385956449 cites W1991466696 @default.
• W4385956449 cites W1993750261 @default.
• W4385956449 cites W2005390110 @default.
• W4385956449 cites W2005420383 @default.
• W4385956449 cites W2006189979 @default.
• W4385956449 cites W2014501567 @default.
• W4385956449 cites W2014677385 @default.
• W4385956449 cites W2023948164 @default.
• W4385956449 cites W2035791702 @default.
• W4385956449 cites W2037173388 @default.
• W4385956449 cites W2039413544 @default.
• W4385956449 cites W2044653660 @default.
• W4385956449 cites W2047620873 @default.
• W4385956449 cites W2072991122 @default.
• W4385956449 cites W2078226889 @default.
• W4385956449 cites W2079826691 @default.
• W4385956449 cites W2081136852 @default.
• W4385956449 cites W2096892888 @default.
• W4385956449 cites W2107538981 @default.
• W4385956449 cites W2118682047 @default.
• W4385956449 cites W2134698251 @default.
• W4385956449 cites W2141442289 @default.
• W4385956449 cites W2144153626 @default.
• W4385956449 cites W2192726575 @default.
• W4385956449 cites W2205491139 @default.
• W4385956449 cites W2279276724 @default.
• W4385956449 cites W2336283051 @default.
• W4385956449 cites W2416755734 @default.
• W4385956449 cites W2527806811 @default.
• W4385956449 cites W2531019859 @default.
• W4385956449 cites W2581398876 @default.
• W4385956449 cites W2618046643 @default.
• W4385956449 cites W2624573876 @default.
• W4385956449 cites W2732794495 @default.
• W4385956449 cites W2745258220 @default.
• W4385956449 cites W2761057337 @default.
• W4385956449 cites W2763159392 @default.
• W4385956449 cites W2887278367 @default.
• W4385956449 cites W2909681691 @default.
• W4385956449 cites W2914982599 @default.
• W4385956449 cites W2922311667 @default.
• W4385956449 cites W2937448484 @default.
• W4385956449 cites W2956035298 @default.
• W4385956449 cites W2966750047 @default.
• W4385956449 cites W2968232462 @default.
• W4385956449 cites W2983067027 @default.
• W4385956449 cites W2990009243 @default.
• W4385956449 cites W2998303347 @default.
• W4385956449 cites W3008847565 @default.
• W4385956449 cites W3022393745 @default.
• W4385956449 cites W3094721985 @default.
• W4385956449 cites W3107728448 @default.
• W4385956449 cites W3110464612 @default.
• W4385956449 cites W3118528518 @default.
• W4385956449 cites W3138652295 @default.
• W4385956449 cites W3163545403 @default.
• W4385956449 cites W3185531925 @default.
• W4385956449 cites W3204207558 @default.
• W4385956449 cites W3207753382 @default.
• W4385956449 cites W4282973773 @default.
• W4385956449 cites W4308915401 @default.
• W4385956449 doi "https://doi.org/10.33933/2713-3001-2023-71-207-230" @default.
• W4385956449 hasPublicationYear "2023" @default.
• W4385956449 type Work @default.
• W4385956449 citedByCount "0" @default.
• W4385956449 crossrefType "journal-article" @default.
• W4385956449 hasAuthorship W4385956449A5067988774 @default.
• W4385956449 hasBestOaLocation W43859564491 @default.
• W4385956449 hasConcept C111368507 @default.
• W4385956449 hasConcept C115343472 @default.
• W4385956449 hasConcept C122523270 @default.
• W4385956449 hasConcept C127313418 @default.
• W4385956449 hasConcept C132651083 @default.
• W4385956449 hasConcept C13280743 @default.
• W4385956449 hasConcept C136894858 @default.
• W4385956449 hasConcept C153294291 @default.
• W4385956449 hasConcept C168754636 @default.
• W4385956449 hasConcept C205649164 @default.
• W4385956449 hasConcept C39432304 @default.
• W4385956449 hasConcept C49204034 @default.
• W4385956449 hasConcept C518008717 @default.
• W4385956449 hasConcept C65440619 @default.
• W4385956449 hasConcept C91586092 @default.
• W4385956449 hasConceptScore W4385956449C111368507 @default.
• W4385956449 hasConceptScore W4385956449C115343472 @default.
• W4385956449 hasConceptScore W4385956449C122523270 @default.
• W4385956449 hasConceptScore W4385956449C127313418 @default.

• next