{"blocks":[{"key":"2n6l0","text":"Regular snowfall over the past week brought about 40-80 cm of snow to the region, with the greatest accumulations focused in the Monashees. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"e1qt5","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"bj06","text":"Elevated, mainly south winds over the same period redistributed much of this snow in the alpine and upper treeline. Warm temperatures promoted slab formation with each snowfall as well as fairly quick transitions to settlement and bonding of the new snow. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"6rhk0","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"bp1r7","text":"Surface snow recently became moist or wet from warm temperatures, wet flurries, or rain up to at least 1500 metres. New melt-freeze crusts may be found on the surface below this elevation, particularly where more pronounced melt occurred.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"49djc","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"7rap1","text":"The layer of surface hoar we have been tracking since late December, now buried 90 to 170 cm deep, has gained considerable strength and is now considered dormant by professionals in the region. It remains a limited concern, potentially triggerable by large loads, in isolated areas of the Selkriks and the northern end of the Monashees. It exists primarily at treeline and just below treeline.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":13,"length":12,"key":0}],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"href":"https://www.avalanche.ca/glossary#surface-hoar","target":"_self","url":"https://www.avalanche.ca/glossary#surface-hoar"}}}}