From 522952651c0f405b734cb1375f3e73c347bb769f Mon Sep 17 00:00:00 2001 From: Ghislain Picard Date: Fri, 16 Sep 2022 15:40:43 +0200 Subject: [PATCH] update changelog --- CHANGELOG.md | 14 +++++++++++--- 1 file changed, 11 insertions(+), 3 deletions(-) diff --git a/CHANGELOG.md b/CHANGELOG.md index 11ecafa..e219bbd 100644 --- a/CHANGELOG.md +++ b/CHANGELOG.md @@ -1,18 +1,26 @@ # Changelog -All notable changes to this project will be documented in this file. +All notable changes to this project are documented in this file. The format is based on [Keep a Changelog](https://keepachangelog.com/en/1.0.0/). ## [Unreleased] ### Added + +### Changed + + +## [v1.1.0] +### Added + - Strong Expansion theory is now implemented in SMRT (see Picard et al. 2022 TC) + - volumetric_liquid_water is a new (and recommended) way to set the amount of water in a layer using make_snowpack. - - the 'emmodel' argument in make_model can now be a dict mapping of different emmodels for each sort of layer medium. Useful for snow + sea-ice for instance when the emmodels must be different for snow and ice. + - the 'emmodel' argument in make_model can now be a dict mapping different emmodels for each sort of layer medium. Useful for snow + sea-ice for instance when the emmodels must be different for snow and ice. - a new function in make_medium.py to create a water body (lake or open ocean): from smrt import make_water_body ### Changed - - Fresnel coefficients for the reflection and transmission on flat interface are now calculated with a more rigorous equation for (very) lossly materials. This could affect some simulations but with very little effect 60°. + - Fresnel coefficients for the reflection and transmission on flat interface are now calculated with a more rigorous equation for (very) lossly materials. This could affect some simulations with water but the effect is most > 60° incidence angle.