Zobrazeno 1 - 10
of 77
pro vyhledávání: '"Andrew Ireson"'
Wetland systems are among the largest stores of carbon on the planet, most biologically diverse of all ecosystems, and dominant controls of the hydrologic cycle. However, their representation in land surface models (LSMs), which are the terrestrial l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e3dcb3a5628f0571dc6935418cce370f
https://doi.org/10.5194/hess-2023-68
https://doi.org/10.5194/hess-2023-68
Autor:
Grant Ferguson, Jared D. Wolfe, Helen M. Baulch, Kenneth Belcher, Phil Loring, John W. Pomeroy, Kevin Shook, Patrick Lloyd-Smith, Masaki Hayashi, Robert G. Clark, Nandita B. Basu, Chris Spence, Angela Bedard-Haughn, Colin J. Whitfield, Andrew Ireson
Publikováno v:
Canadian Water Resources Journal / Revue canadienne des ressources hydriques. 46:229-241
Extensive wetland drainage has occurred across the Canadian Prairies, and drainage activities are ongoing in many areas (Dahl 1990; Watmough and Schmoll 2007; Bartzen et al. 2010; Dahl 2014; Prairi...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19cdc32c7c72c6fc91b2cf2087df6238
https://doi.org/10.1080/07011784.2021.1973911
https://doi.org/10.1080/07011784.2021.1973911
Publikováno v:
Hydrological Processes. 36
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7aeb16668f042d49445bcfceb686f0fa
https://doi.org/10.1002/hyp.14664
https://doi.org/10.1002/hyp.14664
Publikováno v:
Hydrological Processes. 34:927-940
The exchanges of water, energy and carbon between the land surface and the atmosphere are tightly coupled, so that errors in simulating evapotranspiration lead to errors in simulating both the water and carbon balances. Areas with seasonally frozen s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31e89dc0fe204e04ba524d84b1e4a260
https://doi.org/10.1002/hyp.13674
https://doi.org/10.1002/hyp.13674
Publikováno v:
Water Resources Research, 2021, Vol.57(8), pp.e2021WR030070 [Peer Reviewed Journal]
The phenomenon of freezing point depression in frozen soils results in the co-existence of ice and liquid water in soil pores at temperatures below 273.15 K (0°C), and is thought to have two causes: (a) capillary and adsorption effects, where the ph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ec1e4ee58f1d14db3c8db5e7864edee1
https://doi.org/10.1029/2021wr030070
https://doi.org/10.1029/2021wr030070
Autor:
Matthew K. MacDonald, Bruce Davison, Zelalem Tesemma, Fuad Yassin, Saman Razavi, Mohamed Elshamy, Karl-Erich Lindenschmidt, Ala Bahrami, C. M. DeBeer, John W. Pomeroy, Abbas Fayad, Prabin Rokaya, Amin Haghnegahdar, Alain Pietroniro, Daniel Princz, Mohamed S. Abdelhamed, Howard Wheater, Andrew Ireson, Amin Elshorbagy, Youssef Loukili
Cold regions provide water resources for half the global population yet face rapid change. Their hydrology is dominated by snow, ice and frozen soils, and climate warming is having profound effects. Hydrological models have a key role in predicting c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::17cdeec260a925906a725ad52388ac08
https://doi.org/10.22541/au.162738548.88997933/v1
https://doi.org/10.22541/au.162738548.88997933/v1
Publikováno v:
Water Resources Research. 55:4410-4426
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4700cc3e29118ee79c29d9a624eb10fb
https://doi.org/10.1029/2018wr023329
https://doi.org/10.1029/2018wr023329
Autor:
Andrew Ireson, Edward K. P. Bam
Publikováno v:
Journal of Hydrology. 570:185-200
Stable isotopes have been used to quantify lake and wetland pond water loss to evaporation by applying the modified Craig and Gordon (1965) model. This model and its derivatives employ simplifying assumptions that ignore the additions of precipitatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b18ee3184304ef8c413e62d146187dc1
https://doi.org/10.1016/j.jhydrol.2018.12.032
https://doi.org/10.1016/j.jhydrol.2018.12.032