Zobrazeno 1 - 10
of 34
pro vyhledávání: '"C. T. Simmons"'
Autor:
B. Ataie-Ashtiani, C. T. Simmons
Publikováno v:
Hydrology and Earth System Sciences, Vol 24, Pp 761-769 (2020)
We revisit and shed light on the millennium-old hydrogeology textbook The Extraction of Hidden Waters by the Persian mathematician and engineer Karaji. Despite the nature of the understanding and conceptualization of the world by the people of that t
Externí odkaz:
https://doaj.org/article/c358b8c7ddff403e8f7c66adfb7da368
Publikováno v:
Climate of the Past, Vol 9, Iss 4, Pp 1761-1771 (2013)
The end of the Pleistocene was a turning point for the Earth system as climate gradually emerged from millennia of severe glaciation in the Northern Hemisphere. The deglacial climate change coincided with an unprecedented decline in many species of P
Externí odkaz:
https://doaj.org/article/90963d367c6346db98a92f4024a8baa6
Publikováno v:
Hydrology and Earth System Sciences, Vol 14, Iss 7, Pp 1233-1245 (2010)
Of the various approaches for estimating groundwater recharge, the chloride mass balance (CMB) method is one of the most frequently used, especially for arid and semiarid regions. Widespread native vegetation clearance, common in many areas globally,
Externí odkaz:
https://doaj.org/article/6f40371d3371428fa703a2e4258c974f
Publikováno v:
Hydrology and Earth System Sciences, Vol 14, Iss 5, Pp 801-813 (2010)
Chloride is commonly used as an environmental tracer for studying water flow and solute transport in the environment. It is especially useful for estimating groundwater recharge based on the commonly used chloride mass balance (CMB) method. Strong sp
Externí odkaz:
https://doaj.org/article/787fbcb3288e40e095efdc7ce1b5598b
Publikováno v:
Water Resources Research. 58
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0183551ca983842cb06b5a26a98f8251
https://doi.org/10.1029/2021wr031458
https://doi.org/10.1029/2021wr031458
Autor:
C T Simmons, H D Matthews
Publikováno v:
Environmental Research Letters, Vol 11, Iss 3, p 035001 (2016)
Recent research has shown evidence of a linear climate response to cumulative CO _2 emissions, which implies that the source, timing, and amount of emissions does not significantly influence the climate response per unit emission. Furthermore, these
Externí odkaz:
https://doaj.org/article/aa95be10ee1342758c11cd8dfd8f046e
Publikováno v:
Climate of the Past, Vol 9, Iss 4, Pp 1761-1771 (2013)
The end of the Pleistocene marked a turning point for the Earth system as climate gradually emerged from millennia of severe glaciation in the Northern Hemisphere. It is widely acknowledged that the deglacial climate change coincided with an unpreced
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9422b23567c63c71ff7225eb8f3599ee
https://doi.org/10.5194/cp-9-1761-2013
https://doi.org/10.5194/cp-9-1761-2013
Publikováno v:
Atmosphere-Ocean. 51:187-212
The mechanisms behind the 20 ppm pre-industrial rise in atmospheric CO2 since 6000 BC have been the focus of considerable debate in recent years. Some studies suggest that natural processes, such as a decline in global forests, calcite compensation,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2aa4f3fb78cc63352576333eca7d3ae
https://doi.org/10.1080/07055900.2013.773880
https://doi.org/10.1080/07055900.2013.773880
Publikováno v:
Ground water. 55(3)
The rapid expansion in unconventional gas development over the past two decades has led to concerns over the potential impacts on groundwater resources. Although numerical models are invaluable for assessing likelihood of impacts at particular sites,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::a8f07f794034e1d507f82d173bfe0465
https://pubmed.ncbi.nlm.nih.gov/27943264
https://pubmed.ncbi.nlm.nih.gov/27943264
Proxy reconstructions and modeling studies of the glacial-interglacial changes in the global carbon cycle have led to a stimulating debate in the paleoclimate literature about the mechanisms leading to a 90–100 ppmv increase in atmospheric CO2. In
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b74397e14de6dd01380b413b7789e402
https://doi.org/10.5194/cp-2016-24
https://doi.org/10.5194/cp-2016-24
