Cargando…
Climate Change : Identification and Projections.
Under certain scenarios on the subject of CO2 emissions, by the end of the century the atmospheric concentration could triple its pre-industrial level. The very large numerical models intended to anticipate the corresponding climate evolutions are designed and quantified from the laws of physics. Ho...
| Clasificación: | Libro Electrónico |
|---|---|
| Autor principal: | |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
Hoboken :
Wiley,
2014.
|
| Colección: | Focus series.
|
| Temas: | |
| Acceso en línea: | Texto completo |
MARC
| LEADER | 00000cam a2200000Mi 4500 | ||
|---|---|---|---|
| 001 | EBOOKCENTRAL_ocn894791046 | ||
| 003 | OCoLC | ||
| 005 | 20240329122006.0 | ||
| 006 | m o d | ||
| 007 | cr cn||||||||| | ||
| 008 | 141108s2014 xx ob 001 0 eng d | ||
| 040 | |a EBLCP |b eng |e pn |c EBLCP |d RECBK |d DEBSZ |d OCLCQ |d S4S |d OCLCO |d OCLCQ |d OCLCO |d OCLCF |d EBLCP |d OCLCQ |d COCUF |d MOR |d CCO |d PIFAG |d ZCU |d MERUC |d OCLCQ |d U3W |d STF |d ICG |d INT |d AU@ |d OCLCQ |d TKN |d OCLCQ |d OCLCA |d DKC |d OCLCQ |d OCLCO |d SGP |d OCLCQ |d OCLCO | ||
| 066 | |c (S | ||
| 020 | |a 9781119053941 | ||
| 020 | |a 1119053943 | ||
| 020 | |z 9781848217775 | ||
| 029 | 1 | |a CHSLU |b 001175006 | |
| 029 | 1 | |a CHVBK |b 327665564 | |
| 029 | 1 | |a DEBBG |b BV043613359 | |
| 029 | 1 | |a DEBSZ |b 43181743X | |
| 035 | |a (OCoLC)894791046 | ||
| 050 | 4 | |a GE195 | |
| 050 | 4 | |a QC981.8.C5 | |
| 080 | |a 551.583 | ||
| 082 | 0 | 4 | |a 333.72 |
| 049 | |a UAMI | ||
| 100 | 1 | |a De Larminat, Philippe. | |
| 245 | 1 | 0 | |a Climate Change : |b Identification and Projections. |
| 260 | |a Hoboken : |b Wiley, |c 2014. | ||
| 300 | |a 1 online resource (152 pages) | ||
| 336 | |a text |b txt |2 rdacontent | ||
| 337 | |a computer |b c |2 rdamedia | ||
| 338 | |a online resource |b cr |2 rdacarrier | ||
| 490 | 1 | |a Focus ecological science series | |
| 490 | 1 | |a Focus series, |x 2051-2481 | |
| 588 | 0 | |a Print version record. | |
| 505 | 0 | |a Cover; Title Page; Copyright; Contents; 1: Introduction; 1.1. Context; 1.2. Identification; 1.3. Expectations and results; 1.4. Contents of the work; 2: Climatic Data; 2.1. Sources; 2.2. Global temperature; 2.2.1. Modern temperatures; 2.2.2. Pre-industrial temperature; 2.2.3. Paleotemperatures; 2.3. Concentration of CO2 in the atmosphere; 2.4. Solar activity; 2.5. Volcanic activity; 3: The War of the Graphs; 3.1. History; 3.2. Inconsistent controversies; 3.3. Usable data; 4: Formulating an Energy Balance Model; 4.1. State models and transmittance; 4.2. Structure of an energy balance model. | |
| 505 | 8 | |6 880-01 |a 7.1. A selection of data7.2. Free identification; 7.3. Forced identifications; 7.4. Statistical analysis; 8: Overall Results; 8.1. Preliminary comments; 8.2. Regions and intervals of confidence; 8.3. Hypothesis test; 8.4. Comments; 9: Historic Minuscule Simulations; 9.1. Overview of IPCC simulations; 9.2. Comparative simulations; 9.3. Representative concentration pathways (RCPs); 9.4. Comparative radiative forcing; 10: Long-term Climate Projections; 10.1. IPCC scenarios and projections; 10.2. EBM compatible scenarios; 10.3. Long-term projections; 10.4. A disaster scenario. | |
| 505 | 8 | |a 11: Short-term Predictions11.1. Decadal time scale predictions by GCM; 11.2. The climate's natural variability; 11.3. State estimate and prediction; 11.4. Decadal time scale predictions by EBM; 11.5. A posteriori predictions; 12: Conclusions; 12.1. On the identification; 12.2. Climate sensitivity; 12.3. Solar activity; 12.4. Predictive capacity; 12.5. The climate change in question; 12.6. Prospects; Bibliography; Index. | |
| 520 | |a Under certain scenarios on the subject of CO2 emissions, by the end of the century the atmospheric concentration could triple its pre-industrial level. The very large numerical models intended to anticipate the corresponding climate evolutions are designed and quantified from the laws of physics. However, little is generally known about these: genesis of clouds, terms of the greenhouse effect, solar activity intervention, etc. This book deals with the issue of climate modeling in a different way: using proven techniques for identifying black box-type models. Taking climate observations fr. | ||
| 504 | |a Includes bibliographical references and index. | ||
| 590 | |a ProQuest Ebook Central |b Ebook Central Academic Complete | ||
| 650 | 0 | |a Climatic changes. | |
| 650 | 2 | |a Climate Change | |
| 650 | 6 | |a Climat |x Changements. | |
| 650 | 7 | |a climate change. |2 aat | |
| 650 | 7 | |a SCIENCE |x Earth Sciences |x Geography. |2 bisacsh | |
| 650 | 7 | |a SCIENCE |x Earth Sciences |x Geology. |2 bisacsh | |
| 650 | 7 | |a Climatic changes |2 fast | |
| 776 | 0 | 8 | |i Print version: |a De Larminat, Philippe. |t Climate Change : Identification and Projections. |d Hoboken : Wiley, ©2014 |z 9781848217775 |
| 830 | 0 | |a Focus series. | |
| 856 | 4 | 0 | |u https://ebookcentral.uam.elogim.com/lib/uam-ebooks/detail.action?docID=1830138 |z Texto completo |
| 880 | 8 | |6 505-01/(S |a 4.3. Specificity of EBMs4.4. Dynamic parametrization; 5: Presumed Parameters; 5.1. Terminology; 5.2. Climate sensitivity Sclim; 5.3. Coefficient of radiative forcing α1; 5.4. The climate feedback coefficient λG; 5.5. Sensitivity to irradiance S2; 5.6. Sensitivity to volcanic activity S3; 5.7. Climate or anthropogenic sensitivity; 5.8. Review of uncertainties; 6: Identification Method; 6.1. The current state of affairs; 6.2. Output error method; 6.3. Estimating the error variance; 6.4. Hypothesis test and confidence regions; 6.5. Conditions of application; 7: Partial Results. | |
| 938 | |a EBL - Ebook Library |b EBLB |n EBL4040811 | ||
| 938 | |a EBL - Ebook Library |b EBLB |n EBL1830138 | ||
| 938 | |a Recorded Books, LLC |b RECE |n rbeEB00588431 | ||
| 994 | |a 92 |b IZTAP | ||