If you installed ArtCAM 2013 - Full Install (7.14 GB) or ArtCAM 2013 Service Pack 3 - Minimal Install (678 MB) prior to 13th November 2014, please select the Help > Check for ArtCAM Updates > Software Updates menu option in ArtCAM 2013.SP3 (build 298), then proceed to download the ArtCAM 2013.SP3 Tool List Hotfix from the Delcam Customer Download Centre. Alternatively, Verified ArtCAM Users and Verified ArtCAM Express Users can download the ArtCAM 2013.SP3 Tool List Hotfix from the ArtCAM Forum.
If you download and install ArtCAM 2013 - Full Install (7.14 GB) or ArtCAM 2013 Service Pack 3 - Minimal Install (678 MB) from 13th November, it is not necessary to install the ArtCAM 2013.SP3 Tool List Hotfix afterwards, as both have since been modified to include it.
Art Cam 2013 Download
DOWNLOAD: https://tlniurl.com/2vEYMo
Given that the ocean helps set the pace of transient climate change, an interesting follow-up question is this: besides ocean heat uptake, does the ocean impact either equilibrium or transient warming through other mechanisms, such as heat transport? Several studies indicate that poleward ocean heat transport warms the Earth system (Rind and Chandler 1991; Winton 2003; Herweijer et al. 2005; Rencurrel and Rose 2018), suggesting that any changes in ocean heat transport concomitant with CO2 forcing might impact just how much the Earth system warms. Indeed, this sensitivity to changing poleward ocean heat transport is evident in the Arctic: greater poleward ocean heat transport into the Arctic with CO2 forcing is associated with greater sea ice loss, more surface warming, and stronger polar amplification (Holland and Bitz 2003; Mahlstein and Knutti 2011; Hwang et al. 2011; Singh et al. 2017). Other studies suggest that the magnitude of weakening in the Atlantic meridional overturning circulation, which decreases northward ocean heat transport over the Atlantic basin, determines the magnitude of surface warming in the Northern Hemisphere (Rugenstein et al. 2013; Lin et al. 2019; Weijer et al. 2020; Liu et al. 2020).
In each of these experiments, the atmospheric energy transport (AET) response to CO2 doubling opposes the prescribed OHT changes. In experiments with increasing poleward OHT, poleward AET decreases (see red-hued lines, 5b), and in experiments with decreasing poleward OHT, poleward AET increases (see blue-hued lines). Indeed, changes in AET are minimal when there are no prescribed OHT changes (see gray line), presumably because there are no OHT changes to oppose. Compensation between poleward atmosphere and ocean energy transports is unsurprising, and is ubiquitous in climate modeling studies (see, e.g., Bjerknes 1964; Vellinga and Wood 2002; Vellinga and Wu 2008; Kang et al. 2008; Farneti and Vallis 2013). 2ff7e9595c
Comentarios