P0L3/CliReNER_v_1_1_28_SILVER huggingface dataset:
Wild-type strains of white-rot fungi Phanerochaete chrysosporium (PC) Burdsall (ATCC 24725) and Trametes versicolor 52J (Tv 52J) (ATCC 2086), and cellobiose dehydrogenase-deficient strain (mutant) of the basidiomycete Trametes versicolor (Tv m4D) [34] used in this study were supplied by Agriculture and Agri-Food Canada, Saskatoon Research and Development Centre, Canada.
The surface temperature of the Arctic warmed 2 – 3 times faster than the global average for the accelerated change rate of sea ice and surface albedo (Baek et al. 2020; Kato et al. 2018), and the abnormal temperatures have caused a series of extreme weather and climate events worldwide (Coumou et al. 2018; Gramling 2015; Kug et al. 2015; Wu and Smith 2016).
For example, Liu et al. (2010) and He et al. (2019) found that the Arctic cloud coverage from the Moderate Resolution Imaging Spectroradiometer (MODIS) or the – fi(  ) data linearly increased with ice-free water areas from 2006 to 2008, whereas Philipp et al. (2020) found that the summer lowlevel CF has an  insignificant  positive correlation with negative sea ice concentration using the Advanced Very-High-Resolution Radiometer (AVHRR) data.
Additionally, we have explored the EASM variation modulated by the internal climate variability, and there is no 11-yr peak presenting in the power spectrum for the entire 1000-yr CTRL experiment (Fig. 4). 2739 Since abnormal changes in sea surface temperature (SST) may have a significant effect on the EASM circulation and water vapor transport (Wang et al. 2008a; Xu et al. 2016), it is meaningful to examine the SST anomalies associated with an enhanced EASM.
The results shown in Fig. 6 suggest that the regions where the SST responds differently to the strong and weak 11-yr solar cycles are located poleward of 20 N in the North Pacific, and during the peak years with the strong 11-yr solar cycle can induce an SST Meanwhile, the significant 11-yr period is almost not shown in each single solar-only forcing experiment during both the strong and weak 11-yr solar cycle epochs (figure omitted), which may be due to the fact that internal variability dominates each solar-only forcing experiment.
We calculated cloud-reduced, maximum NDVI composites in Google Earth Engine (see Gorelick et al. 2017) for Landsat 8 bands 1–7 plus Enhanced Vegetation Index-2 (EVI2), Normalized Burn Ratio (NBR), Normalized Difference Moisture Index (NDMI), Normalized Difference Snow Index (NDSI), Normalized Difference Vegetation Index (NDVI), and Normalized Difference Water Index (NDWI).
The linear relationship between conductivity and ionic strength, reported by Griffin and Jurinak [21], resulted in ionic strength conditions of 0.06–0.08 M. Therefore, under the temperature and ionic strength conditions measured at the wetland, the solubility of monobasic urate is calculated to range from 0.003 M–0.007 M (or 0.6–1.3 g/L, for monosodium urate).
Mukherjee and Borhad [26] measured the dry masses and contents of excreta for those species; with the assumption that they represent all of those counted at the OEW (Figure 6), an input of 140 kg·day−1 UA (September 2017), 450 kg·day−1 UA (December 2017) and 130 kg·day−1 UA (March 2018) would be added to the park.
With the advent of SPM, however, researchers are presented with an intriguing opportunity to explore subdiffraction limit (or superresolved) vibrational spectroscopy using the AFM tip either as a scattering source (scanning scattering near-field optical microscope [s-SNOM], tip-enhanced Raman [TERS]) or to monitor localized photothermal (PT) expansion–PT-induced resonance (7, 8).