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First 1283 results for ” Sue Ellen Haupt”

1. Tasman leakage: a new route in the global ocean conveyor belt

   The existence of a new route that draws relatively cold waters from the Pacific Ocean to the Nort...

   S Speich, B Blanke, P de Vries, K Doos, SS Drijfhout, A Ganachaud, R Marsh | Status: published | Journal: Geophys. Res. Lett. | Volume: 29 | Year: 2002 | First page: 0 | Last page: 0 | doi: 10.1029/2001GL014586

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2. Photolysis Frequency of 0 3 to 01 (1D): Measurements and modelling during the International Photolysis Frequency Measurement and Modelling Intercomparison (IPMMI)
   A Hozumahaus, BL Lefer, PS Monks, SR Hall, A Kylling, B Mayer, .............................., M van Weele | Status: published | Journal: J. Geophys. Res. | Volume: 109 | Year: 2004 | doi: 10.1029/2003JD004333

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3. Comparison of GOME tropospheric NO2 columns with NO2 profiles deduced from ground-based in situ measurement

   Nitrogen dioxide (NO2) vertical tropospheric column densities (VTCs) retrieved from the Global Oz...

   D Schaub, KF Boersma, JW Kaiser, AK Weiss, D Folini, HJ Eskes, B Buchmann | Status: published | Journal: Atm. Chem. Phys. | Year: 2006 | First page: 3211 | Last page: 3229

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4. Western US high June 2015 temperatures and their relation to global warming and soil moisture

   The Western US states Washington (WA), Oregon (OR) and California (CA) experienced extremely high...

   SY Philip, SF Kew, M Hauser, BP Guillod, A Teuling, K Whan, P Uhe, GJ van Oldenborgh | Status: published | Journal: Clim. Dyn. | Volume: 50 | Year: 2018 | First page: 2587 | Last page: 2601 | doi: 10.1007/s00382-017-3759-x

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5. Simulating hydrological extremes for different warming levels–combining large scale climate ensembles with local observation based machine learning models

   Climate change has a large influence on the occurrence of extreme hydrological events. However, r...

   SM Hauswirth, K van der Wiel, MFP Bierkens, V Beijk, N Wanders | Journal: Frontiers in Water | Volume: 5 | Year: 2023 | First page: 11008108 | doi: 10.3389/frwa.2023.1108108

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