From e0c0f59934317a396e72a51f3347da16bde2aab0 Mon Sep 17 00:00:00 2001
From: unknown <olivier.delaigue@ANPI1430.antony.irstea.priv>
Date: Wed, 2 Nov 2016 13:25:25 +0100
Subject: [PATCH] Accents modified in the DataAltiExtrapolation_Valery()
 documentation, to avoid warnings during the compilation of the manual

---
 man/DataAltiExtrapolation_Valery.Rd | 6 +++---
 1 file changed, 3 insertions(+), 3 deletions(-)

diff --git a/man/DataAltiExtrapolation_Valery.Rd b/man/DataAltiExtrapolation_Valery.Rd
index 6f625a27..16b2c768 100644
--- a/man/DataAltiExtrapolation_Valery.Rd
+++ b/man/DataAltiExtrapolation_Valery.Rd
@@ -1,7 +1,7 @@
 \encoding{UTF-8}
 \name{DataAltiExtrapolation_Valery}
 \alias{DataAltiExtrapolation_Valery}
-\title{Altitudinal extrapolation of precipitation and temperature series described by A. Valéry}
+\title{Altitudinal extrapolation of precipitation and temperature series described by A. Valery}
 \usage{
 DataAltiExtrapolation_Valery(DatesR, Precip, TempMean, TempMin = NULL,
   TempMax = NULL, ZInputs, HypsoData, NLayers, verbose = TRUE)
@@ -37,13 +37,13 @@ list containing the extrapolated series of precip. and air temp. on each elevati
          }
 }
 \description{
-Function which extrapolates the precipitation and air temperature series for different elevation layers (method from Valery, 2010).
+Function which extrapolates the precipitation and air temperature series for different elevation layers (method from Valéry, 2010).
 }
 \details{
 Elevation layers of equal surface are created the 101 elevation quantiles (\emph{HypsoData}) 
 and the number requested elevation layers (\emph{NLayers}). \cr
 Forcing data (precipitation and air temperature) are extrapolated using gradients from Valery (2010).
-(e.g. gradP=0.0004 [m-1] for France and gradT=0.434 [degreC/100m] for January, 1st). \cr
+(e.g. gradP=0.0004 [m-1] for France and gradT=0.434 [°C/100m] for January, 1st). \cr
 This function is used by the \emph{CreateInputsModel} function. \cr
 }
 \author{
-- 
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