Zobrazeno 1 - 10
of 62
pro vyhledávání: '"F. González-Rouco"'
Autor:
A. García-García, F. J. Cuesta-Valero, H. Beltrami, F. González-Rouco, E. García-Bustamante, J. Finnis
Publikováno v:
Geoscientific Model Development, Vol 13, Pp 5345-5366 (2020)
The representation and projection of extreme temperature and precipitation events in regional and global climate models are of major importance for the study of climate change impacts. However, state-of-the-art global and regional climate model simul
Externí odkaz:
https://doaj.org/article/4b85f2a741fb4bcf9c6561707b228fb7
Autor:
F. García-Pereira, J. F. González-Rouco, C. Melo-Aguilar, N. J. Steinert, E. García-Bustamante, P. de Vrese, J. Jungclaus, S. Lorenz, S. Hagemann, F. J. Cuesta-Valero, A. García-García, H. Beltrami
Publikováno v:
Earth System Dynamics, Vol 15, Pp 547-564 (2024)
The anthropogenically intensified greenhouse effect has caused a radiative imbalance at the top of the atmosphere during the industrial period. This, in turn, has led to an energy surplus in various components of the Earth system, with the ocean stor
Externí odkaz:
https://doaj.org/article/b3be9d398c3f4f97b2bb9aa37cf5deab
Publikováno v:
Climate of the Past, Vol 9, Iss 2, Pp 547-565 (2013)
Studies addressing climate variability during the last millennium generally focus on variables with a direct influence on climate variability, like the fast thermal response to varying radiative forcing, or the large-scale changes in atmospheric dyna
Externí odkaz:
https://doaj.org/article/2e428bf4980d4ff1b5a38b69a7668c9d
Autor:
I. Dorado Liñán, U. Büntgen, F. González-Rouco, E. Zorita, J. P. Montávez, J. J. Gómez-Navarro, M. Brunet, I. Heinrich, G. Helle, E. Gutiérrez
Publikováno v:
Climate of the Past, Vol 8, Iss 3, Pp 919-933 (2012)
Past temperature variations are usually inferred from proxy data or estimated using general circulation models. Comparisons between climate estimations derived from proxy records and from model simulations help to better understand mechanisms driving
Externí odkaz:
https://doaj.org/article/f73d4580794e4198a480bb96dbe3d51d
Autor:
F. García-Pereira, J. F. González-Rouco, T. Schmid, C. Melo-Aguilar, C. Vegas-Cañas, N. J. Steinert, P. J. Roldán-Gómez, F. J. Cuesta-Valero, A. García-García, H. Beltrami, P. de Vrese
Publikováno v:
SOIL, Vol 10, Pp 1-21 (2024)
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://doaj.org/article/15cc4934120545af95c5ef9f2d76b516
Publikováno v:
Climate of the Past, Vol 19, Pp 2361-2387 (2023)
The Medieval Climate Anomaly (MCA; ca. 950–1250 CE) and the Little Ice Age (LIA; ca. 1450–1850 CE) were periods generally characterized by respectively higher and lower temperatures in many regions. However, they have also been associated with dr
Externí odkaz:
https://doaj.org/article/661866314a0a4024a1aa26c18c1d1e55
Publikováno v:
Geoscientific Model Development, Vol 15, Pp 7913-7932 (2022)
Estimates of the past thermal state of the land surface are crucial to assess the magnitude of current anthropogenic climate change as well as to assess the ability of Earth System Models (ESMs) to forecast the evolution of the climate near the groun
Externí odkaz:
https://doaj.org/article/2eb3b6d9ecac443085c82115b77709df
Autor:
F. J. Cuesta-Valero, A. García-García, H. Beltrami, J. F. González-Rouco, E. García-Bustamante
Publikováno v:
Climate of the Past, Vol 17, Pp 451-468 (2021)
Energy exchanges among climate subsystems are of critical importance to determine the climate sensitivity of the Earth's system to greenhouse gases, to quantify the magnitude and evolution of the Earth's energy imbalance, and to project the evolution
Externí odkaz:
https://doaj.org/article/c06b639a8bac48deb33a9d0f82496782
Publikováno v:
Climate of the Past, Vol 16, Pp 1285-1307 (2020)
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 (LI
Externí odkaz:
https://doaj.org/article/3f81d481282444f0a30c3d37b9f76b24
Autor:
J. H. Jungclaus, E. Bard, M. Baroni, P. Braconnot, J. Cao, L. P. Chini, T. Egorova, M. Evans, J. F. González-Rouco, H. Goosse, G. C. Hurtt, F. Joos, J. O. Kaplan, M. Khodri, K. Klein Goldewijk, N. Krivova, A. N. LeGrande, S. J. Lorenz, J. Luterbacher, W. Man, A. C. Maycock, M. Meinshausen, A. Moberg, R. Muscheler, C. Nehrbass-Ahles, B. I. Otto-Bliesner, S. J. Phipps, J. Pongratz, E. Rozanov, G. A. Schmidt, H. Schmidt, W. Schmutz, A. Schurer, A. I. Shapiro, M. Sigl, J. E. Smerdon, S. K. Solanki, C. Timmreck, M. Toohey, I. G. Usoskin, S. Wagner, C.-J. Wu, K. L. Yeo, D. Zanchettin, Q. Zhang, E. Zorita
Publikováno v:
Geoscientific Model Development, Vol 10, Pp 4005-4033 (2017)
The pre-industrial millennium is among the periods selected by the Paleoclimate Model Intercomparison Project (PMIP) for experiments contributing to the sixth phase of the Coupled Model Intercomparison Project (CMIP6) and the fourth phase of the P
Externí odkaz:
https://doaj.org/article/5c9c80cff63d4624a1a92dd1f053da40