Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Pedro José Roldán-Gómez"'
The Medieval Climate Anomaly (MCA; ca. 950–1250 CE) and the Little Ice Age (LIA; ca. 1450–1850 CE) periods, generally characterised by respectively higher and lower temperatures in many regions, have also been associated with drier and wetter con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40731f1325bd5a4595dd2a35e32ab5ee
https://cp.copernicus.org/preprints/cp-2023-21/
https://cp.copernicus.org/preprints/cp-2023-21/
Autor:
Félix García-Pereira, Jesús Fidel González-Rouco, Thomas Schmid, Camilo Melo-Aguilar, Cristina Vegas-Cañas, Norman Julius Steinert, Pedro José Roldán-Gómez, Francisco José Cuesta-Valero, Almudena García-García, Hugo Beltrami, Philipp de Vrese
Publikováno v:
eISSN
An assessment of the soil and bedrock thermal structure of the Sierra de Guadarrama, in Central Spain, is provided using subsurface and ground surface temperature data coming from four deep (20 m) monitoring profiles belonging to the Guadarrama Monit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2ad1e1306f21465a034368cd916bacd7
https://doi.org/10.5194/egusphere-2023-462
https://doi.org/10.5194/egusphere-2023-462
Autor:
Camilo Melo‐Aguilar, Fidel González‐Rouco, Norman J. Steinert, Hugo Beltrami, Francisco José Cuesta‐Valero, Almudena García‐García, Felix García‐Pereira, Elena García‐Bustamante, Pedro José Roldán‐Gómez, Thomas Schmid, Jorge Navarro
Publikováno v:
International Journal of Climatology. 42:7516-7534
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::575fb350f52023ecb99e62784d2e9fba
https://doi.org/10.1002/joc.7662
https://doi.org/10.1002/joc.7662
Reconstructions of the Last Millennium (LM) suggest coordinated changes in the hydroclimate of separate regions. This happens in regions of North America, North Africa and Europe for the periods of the Medieval Climate Anomaly (MCA; ca. 950–1250 CE
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e94f52525491aafe8b7591431314f0d4
https://doi.org/10.5194/ems2022-285
https://doi.org/10.5194/ems2022-285
Publikováno v:
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
Climate of the Past, Vol 16, Pp 1285-1307 (2020)
E-Prints Complutense. Archivo Institucional de la UCM
instname
Universidad Complutense de Madrid
Climate of the Past, Vol 16, Pp 1285-1307 (2020)
E-Prints Complutense. Archivo Institucional de la UCM
instname
Simulations of climate of the last millennium (LM) show that external forcing had a major contribution to the evolution of temperatures; warmer and colder periods like the Medieval Climate Anomaly (MCA; ca. 950–1250 CE) and the Little Ice Age (LIA;
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7de33b7ebc578428b43c7e0e9097f7a5
https://doi.org/10.5194/cp-2020-8
https://doi.org/10.5194/cp-2020-8